Virginia Warren: Home Sweet Home

NOAA Teacher at Sea Virginia Warren
Mission: Acoustic and Trawl Survey of Walleye Pollock
Geographical Area of Cruise: Shelikof Strait
on NOAA ship Oscar Dyson
Date: 3/25/2016

Science and Technology Log:

This slideshow requires JavaScript.

 

I created the video below  to document some of my activities aboard the Oscar Dyson during my 2016 Teacher at Sea research trip.

In this video, Virginia opens with exciting footage from the front of the Oscar Dyson’s bow as they transit through Alaska’s Shelikof Strait. Interspersed, she shares various steps involved in processing the fish caught in the survey: sorting the catch by species (0:34), collecting the pollock into bins (1:00), making an incision to determine the sex of the pollock (1:07), measuring the pollocks’ lengths and taking biological samples (1:33), removing the otoliths (2:23 and 3:29), preserving the otoliths for analyzing on shore (3:12), and measuring and recording other fish using the Ichthystick and the CLAMS computer program (3:57). Virginia also takes the opportunity to show off some interesting species—lumpsucker fish (2:18), starry flounder (2:53), and salmon (3:53). Finally, Virginia gives a brief tour of the deck (4:38) and finishes with a photo of her wearing a survival (or “Gumby”) suit (5:02.)

My students know a good bit about my previous Teacher at Sea experience out of Woods Hole, Massachusetts where we used the HabCam to look at the ocean floor. With that knowledge in mind a couple of my students asked me if there was a way that we were able to look at the fish while they were still in the water. The simple answer to that question is yes. While my previous TAS experience used the HabCam, the Oscar Dyson uses a CamTrawl. The CamTrawl is attached to the net and it records pictures as fish enter the  cod end of the net.

AWT001_camtrawl2
Image from the CamTrawl

 

DSC02936
CamTrawl
DSC02920
Nick and Ryan Attaching the CamTrawl to the Net

 

After each trawl we would use custom software written in MATLAB to measure lengths of pollock while they were in the water. This program uses the pictures taken from the CamTrawl during the trawl to measure the length of the fish. The CamTrawl takes two pictures at different angles so that most of the time we can see the same fish from two different angles. Fish length irregularities occur in the MATLAB program when it selects nets or two fish at one time to length, so therefore a person has to go back and check to make sure that the program has selected valid fish to length. As the fish pictures come up on the MATLAB screen the person rating the fish selects the fish when the yellow box around the fish covers most of the fish from both angle camera shots of the CamTrawl.

Untitled
A Screen in MATLAB that Shows Valid Fish Lengths

The above picture shows three different fish that were valid choices for length measurement. The pictures on the left show one camera angle and the pictures on the right show the other camera angle. When both angles have a valid fish with the correct placement of the yellow box, the person selecting the fish will click the fish to tell the program to use that fish in the measurement data.

 

Interview With a NOAA Survey Technician: Alyssa Pourmonir 

Alyssa Pourmonir inside the Wet Lab
Alyssa Pourmonir inside the Wet Lab
  1. How did you come to be in NOAA Corps? (or what made you decide to join NOAA Corps and not another military branch.

I am not in the NOAA Corps, instead I am a civilian government employee under the title of Survey Technician. I was in the US Coast Guard for 3 years where I took many courses related to navigation, leadership, and ship life. I feel my background in the Coast Guard has allowed me to excel in this demanding environment.

  1. What is your educational/working background?

I have been lucky to have the opportunity to be in the Coast Guard which taught me many professional skills and built me up to be stronger and more independent. I also spent an entire summer forecasting for the weather in Pennsylvania. Here I gained an abundance of practice presenting the weather on the green screen and performing on live television for WNEP TV. Before coming to Alaska for this job, I worked as a consultant at NASA Stennis Space Center performing remote sensing analysis of forests using data from the MODIS and VIIRS data.

Academically, I have a BS in Marine Environmental Science from SUNY Maritime College, although most of my college experience took place at the US Coast Guard Academy.

  1. How long have you been in NOAA Corps?

I’m not in the NOAA Corps, but I have worked for NOAA for almost 2 years as a Survey Technician. May 2014 to present.

  1. How long have you been on the Dyson?

June 2014 to present.

  1. How long do you usually stay onboard the ship before going home?

In the past 2 years I have visited my family one time. Partly because I wish to send money home so my family can struggle a little less and hopefully enjoy a life with less debt; especially as my father passes retirement age. He has worked several full time jobs at a time for many years just to support my mom and sisters. Potentially, his work ethic and care giving nature is what I try to embody each day.

  1. Have you worked on any other NOAA ships? If so, which one and how long did you work on it?

Nope

  1. What is your job description on the Dyson?

On the NOAA Oscar Dyson, I am a crew member who acts as a liaison to the scientific personnel on board. I work up to 12 hours each day, 7 days per week maintaining the scientific data, equipment, and lab spaces on board. I also work alongside the scientists, deck department, and bridge watch standers to collect data by completing many different oceanographic or fishing operations.

  1. How is your science job on the Dyson different from the NOAA Scientists that you work with?

As a crew member, I facilitate a positive environment with the needed resources for the scientists to fulfill their data analysis and data collection. I also work alongside the scientists to process the fishing catch in our lab. So you can imagine me suited up with the scientists analyzing the fish’s reproduction development stages and extracting otoliths.

  1. What is the best part of your job?

I get to explore and work in the infamous Bering Sea Alaska, Gulf of Alaska, and Aleutian Island chain which most people can’t even imagine doing. Here in Alaska, I do not have the luxuries found in Continental US, so I believe out here there is a great opportunity for character building. It takes someone pretty amazing to live out here and do what we do.

  1. What is the most difficult part of your job?

Being in remote places and not seeing family or friends, but also being so far away that it is super expensive to try to see them.

  1. Do you have any career highlights or something that stands out in your mind that is exceptionally interesting?

I began my BS absolutely hating biology. I dislike and do not eat seafood. I was skittish and would let my partners do all of the dissections during classes, and I felt that I knew nothing about biology. As a Marine Environmental Science major I decided to take as many biology electives as I could. I went from the lowest grade in my classes to someone who received one of the highest grades in each class. I graduated just one class shy of a minor in Marine Biology and now toss around fish on the NOAA Ship Oscar Dyson, a fisheries research vessel. While my first day I would jump when the fish would move unexpectedly, now I can analyze characteristics of the fish with little alarm and much confidence. It is amazing how I enjoy biology now. I hope to encourage others to confidently try new things, for with a little practice and hard work you may accomplish anything or overcome fears you may not have realized you had.

  1. Do you have any advice for students who want to pursue a career with NOAA?

If you wish to pursue a career with NOAA, be sure to work hard to learn as much as you can, but also come out of your comfort zone to pursue as many volunteer or paid jobs that will give you work experience that correlates with your interests. Time management and resilience is often my secret to success.

Personal Log:

I had a fabulous time aboard NOAA Ship Oscar Dyson and I’m very thankful to NOAA giving me the opportunity to travel to Alaska and learn from their scientists!!!

This slideshow requires JavaScript.

My flight home started on a small plane from Kodiak to Anchorage.

20160324_144957
Ravn Alaska’s Bombardier DHC-8-100

 

After the plane got into the air and was flying away from Kodiak, we were treated to a flyby of the Kodak Harbor and even got to see the Dyson outside of the harbor as we flew away.

20160324_150614
Aerial view of the Kodiak Harbor

We flew into Anchorage, Alaska and I was amazed at the beauty of the mountains in Alaska!

20160324_195443
Mountains Outside the Anchorage, Alaska Airport

A little while before sunset I caught a plane from Anchorage to the Chicago, O’Hare airport. The scenery and sunset leaving Alaska was beautiful!!!! I hope this won’t be the last time I get to come to Alaska, because it is a beautiful, adventure-filled part of the United States.

This slideshow requires JavaScript.

 

It was good to be back on land again when we got back to Kodiak, but I do miss being on the ocean!!

20160324_132915
Bow of the Oscar Dyson
20160324_103709
NOAA Ship Oscar Dyson

 

20160324_103737
Finally back on land in front of the NOAA Ship Oscar Dyson!

This experience was wonderful for me, however for my students this experience was invaluable. I was able to communicate and share my experiences with them through email almost daily and they were also able to read my TAS blogs as they were posted. If they don’t learn anything else from my experiences in Alaska, which I know that they will, I hope they will learn that the world is theirs to explore, study, and learn about no matter how small the town is that they come from!!

Virginia Warren: CLAMS and Trawls March 22, 2016

NOAA Teacher at Sea Virginia Warren
Mission: Acoustic and Trawl Survey of Walleye Pollock
Geographical Area of Cruise: Shelikof Strait
on NOAA ship Oscar Dyson
Date: 3/20/16 – 3/22/16

Data from the Bridge (3/21/16):
Sky: Snow
Visibility: 8 to 10 nautical miles (at one point it was more like 2 to 3 nautical miles)
Wind Speed: 23 knots
Sea Wave Height: 4 – 6 feet
Sea Water Temperature: 5° C (41°)
Air Temperature: 0° C (32° F)
Barometric (Air) Pressure: 994.3 Millibars

Science and Technology Log:
The purpose of this research survey is to collect data on walleye pollock (Gadus chalcogrammus) that scientists will use when the survey is complete to help determine the population of the pollock. This data also helps scientists decide where and when to open the pollock fishery to fishermen. Data collection such as this survey are critical to the survival and health of the pollock fishery.

As I mentioned in a previous blog post, we use an AWT (Aleutian Wing Trawl) to complete the pollock survey. The AWT has two doors that glide through the water and hold the net open. The cod end of the net is where all of the fish end up when the trawl is complete.

awt-model-commented1
Scale model of the Aleutian Wing Trawl (AWT) net courtesy of NOAA Scientist Kresimir Williams (Source: TAS Melissa George)

After the trawl is brought back onto the boat, the cod end of net is dumped onto a hydraulic table. The hydraulic table is then lifted up so that it angles the fish down a shoot into the Wet Lab on a conveyor belt.

 

Once the pollock come through the shoot and onto the conveyor belt, the first thing that we do is pick out every type of animal that is not a pollock. So far we have found lots of eulachons (Thaleichthys pacificus), jellyfish (Cnidaria), isopods, and squid. We have even found the occasional chinook salmon (Oncorhynchus tshawytscha), rock fish (Sebastes spp.), and a lumpsucker (Cyclopteridea). The pollock continue to roll down the conveyor belt into a plastic bin until the bin is full. Then the bin of pollock are weighed.

Contents of the Trawl

This slideshow requires JavaScript.

 

The data from every fish we sample goes into a computer system called CLAMS. CLAMS stands for Catch Logger for Acoustic Midwater Survey. While we are taking samples of the fish our gloves get covered in fish scales and become slimy, so to be able to enter the data into the CLAMS system without causing damage there is a touch screen on all of the computers in the Wet Lab.

 

20160322_161321
CLAMS computer system with a touch screen.

 

Once the pollock are weighed, a sample of the fish are taken to be sexed. To sex the fish, we use a scalpel to slice into the side of the fish. The picture of the chart below shows what we are looking for to determine if a pollock is male or female. Once we know what sex the fish is, we put it into a bin that says “Sheilas” for the female fish and “Blokes” for the male fish.

DSC02989

This chart of the Maturity Scale for Walleye Pollock is hanging in the Wet Lab.

DSC02937
Up-close of the Maturity Scale for female pollock.

DSC02988

Up-close of the Maturity Scale for male pollock.

 

Sexing the fish1

Kim showing Virginia what to look for when sexing the fish.

Once the fish are in their correct male/female bin, they are then measured for their length using an Ichthystick.

The Ichtystick was designed and built by MACE staff Rick Towler and Kresimir Williams who wrote a paper on it: http://www.sciencedirect.com/science/article/pii/S0165783610001517

The Ichthystick has a magnet under the board. When the fish is placed on top of the board, a hand held magnet is placed at the fork of the fish tale. Where the hand held magnet is attracted to the magnet under the board tells the computer the length of the fish and the data is automatically stored in the CLAMS program.

DSC03092
Ichtystick
Starry Flounder Length
Getting the length of the starry flounder using the Ichthystick.

The next station is where the stomach, ovaries, and otoliths are removed from the fish and preserved for scientists to research when the survey is over. The ovaries of a female fish are weighed as well. Depending on the size of the ovaries, they may be collected for further research. Once all of the data has been collected from the fish, a label is printed with the data on it. This label is placed in the bag with the stomach or ovaries sample. Kim completes a special project for this survey. She is a stomach content analysist, so she collects stomachs from a sample of fish that will be taken back to her lab to analyze the stomach content of what she collected. She puts the stomach and the label with the fish’s information, into a bag that is placed in a solution of formalin that preserves the samples.

This slideshow requires JavaScript.

The next step is to get the otoliths out of the fish. A knife is used to cut across the head of the pollock. Otoliths are used to learn the age of the fish. The otoliths are placed in a glass vile that has a barcode number that can be scanned and put with all of the fish’s information in CLAMS. This number is used to keep track of the fish data for when the otoliths get analyzed later on.

Getting the Otoliths

This slideshow requires JavaScript.

We also collect length, weight, sex, and stomach samples from other fish that come up in the trawl as well.

Interview with a NOAA Corps Officer: Ensign Caroline Wilkinson
Caroline is a Junior NOAA Corps Officer on board the NOAA ship Oscar Dyson. She is always very helpful with any information asked of her and always has a smile on her face when she does so. Thank you Caroline for making me feel so welcomed on board the Dyson!

DSC03089
Ensign Caroline Wilkinson

How did you come to be in NOAA Corps? (or what made you decide to join NOAA Corps and not another military branch?

  • I graduated from college in May of 2015. I was looking for a job at a career fair at my school and discovered the NOAA Corps. I had heard of NOAA, but didn’t know a lot about NOAA Corps. I wanted to travel and NOAA Corps allowed me that opportunity. I was unsure what type of work I wanted to do, so I decided to join and explore career options or make a career out of NOAA Corps.

What is your educational/working background?

  • I went to the University of Michigan where I received an undergraduate degree in ecology and evolutionary biology and a minor in physical oceanography.

How long have you been in NOAA Corps?

  • July of 2015 I started basic training. Training was at the Coast Guard academy in a strict military environment. We had navigation and ship handling classes seven hours a day.

How long have you been on the Dyson?

  • I have been here since December of 2015.

How long do you usually stay onboard the ship before going home?

  • We stay at sea for two years and then in a land assignment for 3 years before heading back to sea.

Have you worked on any other NOAA ships? If so, which one and how long did you work on it?

  • Nope, no other ships. I had no underway experience except a five-day dive trip in Australia.

Where have you traveled to with your job?

  • We were in Newport, Oregon and then we went to Seattle, Washington for a couple of weeks. Then we went to Kodiak and then to Dutch Harbor.

What is your job description on the Dyson?

  • I’m a Junior Officer, the Medical Officer, and the Environmental Compliance Officer. As a junior officer I am responsible for standing bridge watch while underway. As a Junior Officer I am responsible for standing 8 hours of watch, driving the ship, every day. As medical officer, we have over 150 drugs onboard that I am responsible for inventorying, administering, and ordering. I also perform weekly health and sanitary inspections and Weekly environmental walkthroughs where I’m looking for any safety hazards, unsecured items, leaks or spills that could go into the water.

What is the best part of your job?

  • Getting to drive the ship.

What is the most difficult part of your job?

  • Being so far away from my family and friends.

Do you have any career highlights or something that stands out in your mind that is exceptionally interesting?

  • During training we got to sail in the US Coast Guard Cutter Eagle. It’s a tall ship (like a pirate ship). We were out for eight days. We went from Baltimore to Port Smith, Virginia and had the opportunity to do a swim call 200 miles out in the Atlantic.

What kind of sea creature do you most like to see while you are at sea?

  • We have seen some killer whales and humpback whale in the bay we are in this morning. We’ve also seen some albatross.

Do you have any advice for students who want to join NOAA Corps?

  • You need an undergraduate degree in math or science. There are 2 classes of ten students a year. Recruiters look for students with research experience, a willingness to learn, and a sense of adventure.
DSC03090
Ensign Caroline Wilkinson at the helm.

 

Personal Log:
I have really been enjoying my time aboard the Oscar Dyson and getting to know the people who are on the ship with me. I love spending time on the Bridge because you can look out and see all around the ship. I also like being on the bridge because I get to witness, and sometimes be a part of, the interactions and camaraderie between the NOAA Corps Officers that drive/control the ship and the other ship workers.

DSC03085
Panoramic view of the NOAA Ship Oscar Dyson‘s Bridge. Look at all of those windows!

 

Arnold and Kimrie are responsible for making breakfast, lunch, and dinner for all 34 people on the Oscar Dyson. They also clean the galley and all of the dishes that go along with feeding all of those people. They probably have the most important job on the ship, because in my previous experiences, hungry people tend to be grouchy people.

20160322_095134
Arnold and Kimrie are the stewards of the Oscar Dyson.

 

We’ve had a variety of yummy dishes made for us while we’ve been at sea. Breakfast starts at 7 a.m. and could include a combination of scrambled eggs, breakfast casserole, French toast, waffles, chocolate pancakes, bacon, sausage, or my personal favorite, eggs benedict.

20160322_070541
Breakfast is served. YUM!!!

Lunch is served at 11 a.m. and seems like a dinner with all of the variety of choices. Lunch usually has some type of soup, fish, and another meat choice available, along with vegetables, bread, and desert. Dinner is served at 5 p.m. and usually soup, fish, and another meat choice available, along with vegetables, bread and desert. I loved getting to try all of the different types of fish that they fix for us and I also really liked getting to try Alaskan King Crab for the first time!!

If you are still hungry after all of that, then there is always a 24-hour salad bar, a variety of cereal, snacks, and ice cream available in the galley. The left-overs from previous meals are also saved and put in the refrigerator for anyone to consume when they feel the need. If we are working and unable to get to the galley before a meal is over, Arnold or Kimrie will save a plate for us to eat when we get finished.

I also tried Ube ice cream, which is purple and made from yams. At first I was very skeptical of any kind of sweet treat being made out of yams, but I was pleasantly surprised that it tasted really good!

DSC02999
Ube ice cream made from yams! Very YUMMY!!!

 

There is even a place to do laundry on this ship, which I was very happy about because fishy clothes can get pretty stinky!

DSC03081
Laundry Room

I can’t end a blog without showing off some of the beautiful scenery that I have been privileged to see on this journey. The pictures below are of the Semidi Islands.

This slideshow requires JavaScript.

 

Virginia Warren: Calibrations, Drills, and Interviews March 19, 2016

NOAA Teacher at Sea Virginia Warren
Mission: Acoustic Trawl Survey of Walleye Pollock
Geographical Area of Cruise: Shelikof Strait
on NOAA ship Oscar Dyson
Date: 3/17/16 – 3/18/16

Data from the Bridge:
Sky: Cloudy
Visibility: 10 Nautical Miles
Wind Direction: 0.2 (20°) From the Northeast
Wind Speed: 25 Knots (30 Knots at point during the day)
Sea Wave Height: 5 – 6 ft. on average (10 ft. at highest)
Sea Water Temperature: 5.6° C (42.08° F)
Dry Temperature: 4° C (40° F)
Barometric (Air) Pressure: 1018.4

Science and Technology Log:
When the wind picked up, it was decided that the ship would quit fishing and running transect lines with the echo-sounder and instead go into one of Kodiak’s bays to seek protection from the weather (>40 knot winds and 16 – 20 foot sea waves were forecast). While were were ‘hiding’, the ship’s crew had time to fix a trawl winch problem and change nets, and the scientists conducted a calibration of the echo-sounder (this is done at the beginning and end of surveys). When we left the transect line, we went through Alitak Bay and stopped the ship in front of Hepburn Peninsula, with Deadman Bay to the left of the peninsula and Portage Bay to the right (if you are looking at the map). Where the ship was sitting, the bay was 74.8 m (245.4068 ft) deep and 5.6° C (42.08° F). It was still pretty windy (15-20 knots), but the Hepburn Peninsula blocked us from a lot of the wind.

This slideshow requires JavaScript.

DSC02951
Deadman Bay to the left of Hepburn Peninsula and Portage Bay to the right

The calibration process of the echo sounder took some time. The science crew before me already started the process of calibrating the echo sounder before it was time for my shift to take over. They used three down riggers to send three lines under the center of the boat, where the echo sounder is positioned. A calibration sphere was placed a little further down one of the lines. There is also a lead weight put at the end of the line so that it will help hold the calibration sphere in place as the current moves.

tomichFig1
Echo Sounder Calibration Diagram (Source Credit: Sea Technology Website)

Then one of the science crew uses a system to align the calibration sphere with the echo sounder. There are two types of calibration spheres that we used today. The first, and smaller one, was made out of a tungsten-carbide alloy.

patrick-with-sphere1_small
Patrick holding the Tungsten-Carbide Calibration Sphere (photo by Julia Harvey, TAS summer 2013 DY1307)

The second calibration sphere was larger than the first and it was made out of solid copper. This made for a very easy, get a blog done, day for me because the job was completed by the lead scientist Patrick and Robert, one of the other science crew members.

DSC02956
Robert Putting the Copper Calibration Sphere on the Line

 

Echosounder calibration screen
Echo-sounder display during calibration. On the echogram (depth on vertical axis, time on horizontal axis) you can see the calibration spheres hanging below the ship above the seafloor. (credit: Patrick Ressler)

 

x6602ebs

Diagram to Describe Echo Sounder Technology (Source Credit: FAO Website)

x6602ebt
Diagram to Describe Echo Sounder Technology (Source Credit: FAO Link)

 

 

Interview with a Scientist: Kim
For this leg of the research cruise Kim is on the same shift that I work on and she’s also my roommate. She has been great in helping me get accustomed to sea life and training me on what to do while we are sorting trawls in the science lab. She also agreed to let me interview her to share her story with my students. I am extremely grateful for all of the help, training, and friendship she has provided while I have been on the Dyson. Her interview is below:

IMG_0399
Kim Holding a Smooth Lumpsucker from a Bottom Trawl Survey (photo credit: Kim)

What is your educational background?
I have a bachelor’s of science degree aquatic and fishery sciences and a minor in marine biology.

How long have you been working as a scientist?
About 10 years.

How long have you been working as a NOAA contractor?
6 years.

What is your job description?
I am a stomach content analyst.

How often do you go on a survey?
Usually twice during the summer for about three weeks at a time.

What is a highlight for you while at sea?
A family of 4 got lost at sea and had been missing for 60 hours. We were out on survey and came across them in their life raft. We were able to pull them out. They wrote a book about it called “Lost in the Shelikof: an Alaskan Family’s Struggle to Survive”.

If you would like to read more about this story, here is the link to the book:  http://www.amazon.com/Lost-Shelikof-Alaskan-Familys-Struggle/dp/145650584X

What made you want to be a scientist?
I spent a lot of time on the water as a kid crabbing and playing in the water. I was always drawn to sea life and I wanted to learn as much about it as I could.

What enjoy most about being a scientist?
The survey work is my favorite part of my job. You get to see a lot of unique species that most people don’t get to see. A lot of deep water species. I also like going out on survey because most of my work is done in the lab looking at samples under a microscope. It’s refreshing to be able to travel up here and work on a boat every summer. Sometimes when I’m out here I stop and think “I can’t believe this is my job.” I learn something new every time I come out here. It’s hard work, but it’s also a lot of fun.

What is the hardest part of your job?
We have a sampling plan that tells us what species and what size range of fish we want to collect stomachs from. It can be difficult to get stomachs from all the fish that you’d like to simply because the net doesn’t catch individuals of a certain size. Fish frequently regurgitate their food when they come up in the net and it can be a challenge sometimes to find ones that haven’t thrown up.

What is your favorite sea creature?
Cuttlefish, they are pretty cute.

Here is a short YouTube video about cuttlefish if you would like to see what they look like and how they act: https://www.youtube.com/watch?v=E-zodF-XrSE

Any advice for people who want to be a scientist?
Volunteer as much as you can. Internships, especially those involving field work, are a great way to gain experience and help you decide what aspects of a particular field of science you’re most interested in. Also, having enthusiasm for the work that you’re doing goes a long way towards helping you get possible internships and job opportunities in the future. Hard work and enthusiasm are what helped me get where I am today in my career.

Personal Log:
For the first couple of days on board the Dyson we had beautiful weather blue skies, pretty clouds, beautiful scenery, and calm seas. However, experiencing calm seas came to a halt on Thursday. The wind picked up which caused the ship to rock back and forth with the waves. Gusts of wind would cause water to splash over the bow of the ship, creating a very entertaining show. I loved to watch the waves move and feel the ship’s reaction to the power of the water. When I went to visit the bridge of the ship one wave hit the boat hard enough to ring a bell that is hanging in the bridge. Sitting down to do work or eating a meal can be kind of fun when the wind is up. It’s almost like a roller coaster, because you never know when your chair is going to slide sideways. Walking while the ship was rocking was also interesting because two normal steps could become 5 so that you can keep your balance and stay on your feet.

This slideshow requires JavaScript.

On Friday we had our mandatory at sea drills. The first was a fire drill which was very easy for me because all I had to do for that drill was meet up with the rest of the science crew in a preplanned muster station. The next drill was a little more eventful. We had to bring a survival suit, a life jacket, a hat, and gloves to the preplanned muster station. Once we were there roll was called to make sure we were in the correct station to get on the correct life raft should it became necessary. This part wasn’t too bad because the scenery outside was very pretty. However, after that part was complete the people new to the ship had to put on the survival suit, which is supposed to take less than a minute to put on. This was my first attempt to get into a survival suit and I needed a lot of guidance from ENS Ben Kaiser, one of the NOAA Corps officers. He was very patient with me and also took my picture when I was finally able to get it on.

DSC02993
My First Time in a Survival Suit

 

The Oscar Dyson takes safety very seriously!!

This slideshow requires JavaScript.

 

Virginia Warren: Life at Sea is GREAT!! March 15, 2016

NOAA Teacher at Sea Virginia Warren
Mission: Acoustic and Trawl Survey of Walleye Pollock
Geographical Area of Cruise: Shelikof Strait
on NOAA ship Oscar Dyson
Date: 3/15/2016

Data from the Bridge:
Sky:  Light and variable
Visibility: 10+ Nautical Miles
Wind Direction: West
Wind Speed: 2.50 (4 knots)
Sea Wave Height:  1 – 2, light swell
Air Temperature: 4.2 degrees C (40 degrees F)
Barometric Pressure: 1004.8

 

NOAA and NOAA Corps Information:

NOAA is an acronym that stands for National Oceanic and Atmospheric Administration. NOAA is a government agency that helps keep citizens informed on weather conditions and the climate. It also conducts fisheries management, and coastal restoration. As stated on their website, NOAA’s mission is to understand and predict changes in climate, weather, oceans, and coasts, to share that knowledge and information with others, and to conserve and manage coastal and marine ecosystems and resources. NOAA has nine key focus areas, 12,000 NOAA personnel, and 6,773 scientists and engineers.

If you would like to read more about what NOAA does, please check out their website here: http://www.noaa.gov/about-our-agency

The NOAA Commissioned Corps Officers are in charge of running NOAA ship Oscar Dyson. The officers keep the ship functioning properly and the people safe. The NOAA Commissioned Officer Corps is one of the seven uniformed services of the United States. As stated on the NOAA Corps website, the NOAA Corps mission is to provide officers technically competent to assume positions of leadership and command in the National Oceanic and Atmospheric Administration (NOAA) and Department of Commerce (DOC) programs and in the Armed Forces during times of war or national emergency.  If you would like read more about what the NOAA Corps does, please check out their website here:  http://www.noaacorps.noaa.gov/about/about.html

You can also watch the NOAA Corps Recruitment video here: http://www.noaacorps.noaa.gov/audiovideo/noaacorps_video.html

 

Science and Technology Log:

This is my second full day on the ship and my science crew has sorted three trawls. On the first day on shift, I learned that there is a lot of waiting to get the fishing pollock job done correctly. The Chief Scientist, Patrick, is responsible for choosing where and when to launch the trawl. He does this by watching data on a screen that comes from the echo sounder, which is placed under the ship. When you see bright red color on the screen, then you know there is something registering on the echo sounder. This part of the process can take several hours.

Echo Sounder Screen
Echo Sounder Screen

Once you find the fish, then you have to launch the trawl net. This is a very intricate process because as the net is being launched, it has to be kept free of tangles. If tangles occur in the net it could cause the net to rip once the trawl has begun. At the mouth of the trawl where the opening is for fish to enter, there are two large trawl doors that glide through the water like airplane wings, except the “lift” is a spreading force that goes sideways to open the mouth of the trawl for fish to enter.

awt-model-commented1
Scale model of the Aleutian Wing Trawl (AWT) net courtesy of NOAA Scientist Kresimir Williams

 

Once the trawl is complete, the catch is dumped onto a table that lifts up to the conveyor belt where we separate pollock from all the other types of animals. The pollock are placed into baskets where they are then weighed. A sample of pollock is taken to examine further. Data on everything that we catch goes into a computer system called CLAMS, which is an acronym for Catch Logger for Acoustic Midwater Survey. I will further explain the sorting and data collection processes, and the CLAMS program on a future blog.

This slideshow requires JavaScript.

Personal Log: 

I’m happy to report that all of my flights went great and my luggage didn’t get lost on my way to Kodiak, Alaska. I spent Friday and Saturday nights in Kodiak waiting to rendezvous with the NOAA ship Oscar Dyson Sunday morning.

This slideshow requires JavaScript.

Kodiak is a beautiful, scenic fishing community. I love that Kodiak is able to use clean, alternative-renewable energy resources to make their energy for the island. Notice the wind turbines in the picture below, however Kodiak also uses hydroelectric dams to make most of their power.

Wind Powered Turbines
Wind Powered Turbines

The Oscar Dyson anchored up outside of the Kodiak harbor in efforts to save time by not having to completely dock up in the harbor. The Dyson sent out its small boat called “The Peggy D” to take people to and from the ship. We put really warm jackets that also served as life jackets(float coats).

The "Peggy"

I loved this boat ride because it gave me a view of the harbor I hadn’t been able to see yet!

Beautiful Mountains from the Harbor in Kodiak, Alaska
Beautiful Mountains from the Harbor in Kodiak, Alaska

My first view of the Oscar Dyson was spectacular. I saw it as we rounded a very small island outside of the harbor. With the mountains in the background, the ship made a pretty picture.

NOAA Ship Oscar Dyson
NOAA Ship Oscar Dyson

This is only the beginning of the trip and I am so looking forward to experience the rest of it.

This slideshow requires JavaScript.

 

Virginia Warren: All My Bags are Packed, I’m Ready to Go!!! March 9, 2016

Hi! My name is Virginia Warren. I teach 5th Grade math and science at Breitling Elementary School in Grand Bay, Alabama. I have been a teacher for 6 years. I am currently in the process of going back to graduate school at the University of South Alabama to get my Master’s Degree in Instructional Design and Development.

I am set to fly out of Pensacola, Florida this coming Thursday morning. I will have a short layover at the Dallas Fort Worth Airport in Texas.Then, I will be off again to Seattle, Washington where I will stay the night before finishing my journey the next day. I am excited about getting to spend even a short amount of time in Seattle because I have never been on the West Coast of the United States. I plan to get as much sight seeing in as possible before my flight to Anchorage, Alaska the next morning. Once I get to Anchorage, I will catch another plane to Kodiak, Alaska where I will rendezvous with the rest of the science crew and the NOAA Ship Oscar Dyson on Saturday.

Flight Diary
This image is created from http://flightdiary.net/ and it depicts the flights that I will take to get to Kodiak, Alaska.

 

This will be my second NOAA Teacher at Sea opportunity. In the summer of 2013 I participated in a sea scallop survey on the Research Vessel Hugh R. Sharp. As a teacher this experience has become invaluable to me because it made scientific research come alive to me in way that I had never been able to express to my students prior to this experience. I am extremely excited about having a second opportunity to travel the world and learn about real data research. I am also excited to be able to share this trip with my 5th grade students back home in Grand Bay, Alabama.

edited2 without man behind me.jpg
This picture is from my first NOAA Teacher at Sea research cruise in 2013 aboard the R/V Hugh R. Sharp

I will spend about 2 weeks aboard the NOAA Ship Oscar Dyson participating in an acoustic-trawl survey to estimate pollock abundance in Shelikof Strait.

 

 

 

 

Susy Ellison, So You Want to be a Hydrographer? November 5, 2013

NOAA Teacher at Sea
Susy Ellison
Aboard NOAA Ship Rainier
September 9 – 26, 2013

 

Mission:  Hydrographic Survey
Geographic Area:  Carbondale, CO
Date:  November 5, 2013 

Weather:  You can go to NOAA’s Shiptracker (http://shiptracker.noaa.gov/) to see where the Rainier is and what weather conditions they are experiencing while I am back at school in Glenwood Springs, CO.
GPS Reading: 39o 24,13146 N  107o 12.6711 W
Temp:  -8C
Wind Speed: 0
Barometer: 1026.00 mb
Visibility:  Clear 

Science and Technology Log

How do you become a hydrographer?  After spending 2 ½ weeks aboard the Rainier as a Teacher at Sea, I found that this question had as many answers as the ship had hydrographers.  In fact, if you take time to concatenate the data (obviously, I have become fond of my newest vocabulary word!), you will learn that being a hydrographer is incredibly multi-faceted and is a confluence of ocean-, cartographic-, and computer-based sciences, with some outdoor skills thrown in for good measure. 

Cdr Rick Brennan and some of the hydrographers of the future in Cold Bay, Alaska
Cdr Rick Brennan and some of the hydrographers of the future in Cold Bay, Alaska

The Rainier’s CO, Commander Rick Brennan, finished college with a degree in Civil Engineering.  In 1991, his senior year, he discovered NOAA when a professor suggested he check out the NOAA Corps during a recruiter’s visit to campus. He started as a NOAA Corps member in 1992 and has been involved in hydrographic survey work ever since.  His studies in the NOAA Corps training included coursework on ships, radar, and navigation, and led to his appointment as Commanding Officer (CO) of the NOAA Ship Rude (http://www.moc.noaa.gov/Decomm Ships/ru-index.html). This ship was NOAA’s smallest hydrography vessel at only 90’ long. 

Commander Brennan has seen many changes in hydrography during his career.  First and foremost, has been its evolution as an academic discipline.  The University of New Hampshire, based in Durham, NH, founded the Center for Coastal and Ocean Mapping in 1999.  Their Joint Hydrographic Center was created through a partnership between the University and NOAA.  (http://ccom.unh.edu/about-ccomjhc, http://www.eos.sr.unh.edu/) Prior to this, hydrography was part of more general courses in oceanography.  Now, you can get a Master’s Degree in Hydrography.

The last 20+ years have also seen significant changes in hydrographic technology, especially in the tools used to map the ocean floor.  Prior to 1994, hydrographic vessels were outfitted with single beam sonar, instead of the multi-beam sonar that is today’s standard.  The single beam only provided bathymetric data at a single position on the seafloor directly below the vessel, while multi-beam sonar can give us high resolution information about the seafloor across a swath of the seafloor stretching several hundred meters to either side of the vessel.  The Rainier, as NOAA’s premier hydrography vessel, was fully outfitted with multi-beam sonar by 1998. Other technological advances have included significant changes in information processing, from the days of paper tape and punch card programming, to the development of  hydrography-specific data analysis programs such as CARIS. 

While data collection capabilities have changed exponentially over the past 20 years, CDR Brennan noted changes in how that data is used.  NOAA has set the industry standard worldwide for collecting hydrographic data.  Departments within NOAA are able to use that data to more than make charts. Fisheries biologists can use the detailed seafloor information in their assessments of ecosystem health and the availability of suitable prey species for all parts of the complex ocean-based food web. Shorelines are dynamic; charting plays a role in establishing baseline data in a changing world. Brennan foresees a future where navigators will view charts using a variety of platforms besides merely lines on paper; this will take educating mariners in how to utilize some of the new electronic tools that are available.

Brennan reflected that, while there have been significant advances in the field of hydrography, there is still much work to do.  NOAA publishes an annual review of its hydrographic survey goals (http://www.nauticalcharts.noaa.gov/hsd/NHSP.htm) .  While this might not sound like the most scintillating of reads, it’s a fascinating look at the enormity of the concept of charting our coastline.  Depending on how you view coastline—is it a smoothed-out line of the coast, does it include all the ins and outs and bays, or does it include all the United States’ navigable coastline extending out 200 nautical miles—one thing is certain, there’s a lot of it.  In Alaska, alone, NOAA has identified 324,465 square nautical miles as Navigationally Significant.  The identified total for all of the United States, including the Caribbean, is 511, 051 square nautical miles.  Alaska is big!  The crew of the Rainier will have plenty of work!

Chief Surveyor Jim Jacobsen at work in the computer lab
Chief Survey Technician Jim Jacobson at work in the computer lab

Chief Survey Technician Jim Jacobson’s favorite area to survey is Southeast Alaska with its varied topography, underwater features, and interesting ports.  He should know, since he’s been a member of the Rainier’s survey crew since 1990.  Jim graduated from the University of Washington with a degree in Oceanography—at that time there were no hydrography-specific programs. When he began, a large part of the training consisted of good old, OJT—on the job training, learning new skills as new equipment and techniques became available.  Needless to say, there have been more than a few changes over the past 20+ years.

Jim began his career before GPS was a part of hydrographic survey.  Setting benchmarks to establish sea levels was done using transits and theodolites, triangulating from known points on land to establish location and elevation on shore.  Information was transmitted using microwave towers that were erected on site.  Fast forward to 2013, where GPS is part of everyone’s vocabulary and the ability to know ‘exactly’ where you are is often in the palm of your hand.  The Rainier’s tide gauge stations are set using GPS units that can identify location and elevation to within centimeters.

He also began his career using single beam sonar, instead of today’s multi-beam.  While single beam doesn’t have the pinpoint accuracy that multi-beam sonar might offer, there were a few advantages.  It was a faster way to collect data, since you weren’t collecting as much information with each ‘ping’.  Thus, you could complete more ‘sheets’ (an identified area for mapping) during your time at sea.

Hydrographic survey techniques have changed over time.
Hydrographic survey techniques have changed over time.
http://www.nauticalcharts.noaa.gov/mcd/learnnc_surveytechniques.html

There have been incredible advances in data analysis since Jim started on the Rainier.  Data collected each day has become more complex, requiring more hours of ‘cleaning’ to remove extraneous pings and information.  Hydrographers use increasingly complex computer software to produce charts, often spending up to 5 hours to process one hour’s data.

What’s next?  Jim imagines a future with underwater mapping done by ROVs, remotely operated vehicles, cruising the seafloor to send back terabytes of information.  ROVs are already used in a variety of information-gathering capacities, sending back high-quality video of seafloor conditions, information on water chemistry, or video of marine life from far below the surface.

Here's what hasn't changed--hydrographers work in all sorts of weather and ocean conditions!
Here’s what hasn’t changed–hydrographers work in all sorts of weather and ocean conditions!

Christi Reiser didn’t start out planning to be a hydrographer.  She has, perhaps, the most diverse resume of any of the survey team.  Christi is currently a college student, and will be receiving her BA in Geography from the University of Colorado, Denver at the end of this year.  Her hydrography career began in May, 2012 when she was hired as an intern on the Rainier, earning college credit while working for NOAA.

Christi Reiser
Christi Reiser

Since high school, Christi has earned an Associate’s Degree in Business, was employed as a saddle maker in Austria, and worked for an oil company as a mapping technician.  While all of those pathways gave her something to ponder, it was the GIS part of her mapping job that really ignited the fire that sent her back to college to pursue a degree in Geography with a focus on GIS and a minor in Environmental Science.  To further stoke that fire, Christi worked to design and pursue an internship experience that would allow her to ‘test drive’ a career combining GIS, hydrography, and life on the high seas.  Through a combination of motivation, Google-based searching, a diverse and applicable set of educational and experiential skills, and the courage to make some phone calls and take a few risks, Christi ended up on the Rainier, working as a paid intern. How cool is that?  She earns college credit, gains expertise working with challenging software and data acquisition programs and equipment, charts the uncharted ocean floor, and sees parts of Alaska that aren’t on the usual tourist’s destination list.  One of her projects during her first season on the Rainier was the creation of an online blog describing her work.  You can check it out at http://rainierinternship.blogspot.com/

Through her internship Christi has found that NOAA is one of the most education-oriented organizations she has worked for, constantly providing opportunities to learn new skills and information. She is excited to be working in a GIS-based field and considers it to be one that is ‘never-ending’, since only 4% of the sea floor has been mapped!  After graduation, her next step may be a Master’s Degree in Geography, to add more science research experience to her knowledge base.  After that?  Well, all I can say is that Christi plans to create a new job that “doesn’t even exist”.  Stay tuned.

So, the next time you’re talking to your guidance counselor about college plans, or wondering what you might want to be when and if you grow up, consider the field of hydrography.  Where else do you get to wear a life jacket to work?

Field Operations Officer  (FOO)Meghan McGovern  goes over the Plan of the Day
Field Operations Officer (FOO)Meghan McGovern goes over the Plan of the Day.  Where else do you get to wear a life jacket to work?

Personal Log

Now that I’ve been home a few weeks, it’s time to reflect on my Teacher at Sea experience.  I’ve been asked, more than once, “Did it meet my expectations”?  That’s an easy question to answer—the answer is “No, it exceeded my expectations!”  I came away from my time on the high seas with much more than just knowledge of the complexities of seafloor mapping.  As a firm believer in the concept that ‘everything is interesting’, it would be hard to point to any aspect of my trip that wasn’t something fun and interesting to learn!

The science of hydrography is amazing.  Just thinking about mapping something that you can’t actually see is an incredible concept.  I have always been fascinated with maps and the process of creating a map, but I look at those maps a little differently now, going beyond the story the map tells to thinking about how that map was made. The science of mapping has undergone many changes since those first sailors with their lead lines creating maps of harbors and shorelines.  In case you’re still wondering why hydrography and the Rainier’s mission is so important, check out this clip from a PBS special that aired in September–http://www.pbs.org/newshour/bb/climate-change/july-dec13/arctic_09-17.html

The teamwork, efficiency, and camaraderie on the ship were a common thread uniting each day’s activities.  Each crew member played a role in the success of the ship’s mapping mission. It took everyone from the engine room to the bridge to keep it all ‘shipshape’.  There was really no job too small—everything and everyone had a necessary role. I especially appreciated the fact that every crew member was willing to answer the myriad questions I had;  from specific questions about their job to questions about  how they ended up on the Rainier.

rainbow cb1
Perhaps we should have used some of our sonar capabilities to search for the pot of gold at the end of this rainbow!

At the end of my Teacher at Sea experience I have to conclude that NOAA is one of our country’s best kept secrets.  What other federal agency can bring you such treats as the daily weather report or tide predictions for an entire year, monitor fisheries along our coastal areas, keep track of our changing climate, or survey marine mammals? Of course, you shouldn’t forget all those nautical charts produced by the hydrographers on the Rainier. NOAA’s webpage says it all (http://www.noaa.gov/); from the ocean floor to the top of our atmosphere—and everything in-between. In a world with a rapidly changing climate I can’t think of an agency that is doing more important work.

Many thanks to NOAA and the Teacher at Sea program for providing me with this incredible learning experience.

Even the plates have the NOAA logo!!
Even the plates have the NOAA logo!!

Louise Todd, From the Bridge, September 26, 2013

NOAA Teacher at Sea
Louise Todd
Aboard NOAA Ship Oregon II
September 13 – 29, 2013

Mission: Shark and Red Snapper Bottom Longline Survey
Geographical Area of Cruise: Gulf of Mexico
Date: September 26, 2013

Weather Data from the Bridge:
Barometric Pressure: 1012.23mb
Sea Temperature: 28.4˚C
Air Temperature: 29.6˚C
Wind speed: 6.43knots

Science and Technology Log:

This morning I went up to the bridge to learn about how the NOAA Corps Officers and the Captain navigate and maneuver the Oregon II.  Ensign Rachel Pryor, my roommate, and Captain Dave Nelson gave me a great tour of the bridge!

The Oregon II is 172 feet long and has a maximum speed of 11 knots.  It was built in 1967.  It has two engines although usually only one engine is used.  The second engine is used when transiting in and out of channels or to give the ship more power when in fairways, the areas of high traffic in the Gulf.  The Oregon II has a draft of 15 feet which means the hull extends 15 feet underneath the water line.  My stateroom is below the water line!  Typically the ship will not go into water shallower than 30 feet.

The bridge has a large number of monitors that provide a range of information to assist with navigation.  There are two radar screens, one typically set to a range of 12 miles and one typically set to a range of 8 miles.  These screens enable the officer navigating the ship to see obstructions, other ships and buoys.  When the radar picks up another vessel, it lists a wealth of information on the vessel including its current rate of speed and its destination.  The radar is also useful in displaying squalls, fast moving storms,  as they develop.

Radar Screen
The radar screen is on the far right

Weather is constantly being displayed on another monitor to help the officer determine what to expect throughout the day.

The Nobeltec is a computerized version of navigation charts that illustrates where the ship is and gives information on the distance until our next station, similar to a GPS in your car.  ENS Pryor compares the Nobeltec to hard copies of the chart every 30 minutes.  Using the hard copies of the charts provides insurance in case the Nobeltec is not working.

Charts
Navigation charts

When we arrive at a station, the speed and direction of the wind are carefully considered by the Officer of the Deck (OOD) as they are crucial in successfully setting and hauling back the line.  It is important that the ship is being pushed off of the line so the line doesn’t get tangled up in the propeller of the ship.  While we are setting the line, the OODis able to stop the engines and even back the ship up to maintain slack in the main line as needed.  Cameras on the stern enable the OOD to see the line being set out and make adjustments in the direction of the ship if needed.  The same considerations are taken when we are hauling back.  The ship typically does not go over 2 knots when the line is being brought back in.  The speed can be reduced as needed during the haul back.  The OOD carefully monitors the haul back from a small window on the side of the bridge.  A lot of work goes into navigating the Oregon II safely!

Personal Log:

I was amazed to see all the monitors up on the bridge!  Keeping everything straight requires a lot of focus.  Being up on the bridge gave me a new perspective of all that goes into each station.  We wouldn’t be able to see all of these sharks without the careful driving from the OOD.

The water has been very calm the past few days. It is like being on a lake.  We’ve had nice weather too!  A good breeze has kept us from getting too hot when we are setting the line or hauling back.

Did you Know?

The stations where we sample are placed into categories depending on their depth.  There are A, B and C stations.  A stations are the most shallow, 5-30 fathoms.  B stations are between 30 and 100 fathoms.  C stations are the deepest, 100-200 fathoms.  One fathom is equal to 6 feet.  A fathometer is used to measure the depth.

Fathometer
The fathometer is the screen on the left

John Clark,Headed Home Early, October 1, 2014

NOAA Teacher at Sea
John Clark
Aboard NOAA Ship Henry B. Bigelow
September 23 – October 4, 2013

Mission: Autumn Bottom Trawl Survey
Geographical Area of Cruise: North Atlantic
Date: October 1, 2013

Science and Technology  Log 

A few hours into our shift midnight we get the word we have been expecting for several days – government shutdown. Our mission will be cut a few days short. That reality means the Bigelow has 24 hours to return to its homeport of Newport,  R.I.  It takes us 10 hours and we dock around 1 in the afternoon. With our fisheries operations suddenly declared over comes clean-up time, and we spend the next 6 hours of our shift cleaning up the on‐board fish lab. It is a time consuming but important process. The lab needs to be spotless and “fish scent” free before we can call our work finished on this cruise.  The lab is literally solid stainless steel and every surface gets washed and suds downed so there is no residue remaining.

Eau de fishes
Fish scales hiding under a flap!

Our work is inspected by a member of the crew. If it were the military, the officer would have had white gloves on I believe, just like in the old movies, rolling his finger over a remote spot looking for the dust we missed. But this is a shining stainless steel fish lab so there are two simultaneous inspections going on at once – the one with the eyes and the one with the nose.  It takes us twice to pass the visual inspection as small collections of fish scales are spotted in a few out-of‐the way areas. It takes us one more pass to clear the smell inspection. Up and down the line we walk, we can all smell the faint lingering perfume of “eau de fishes,” but we are having trouble finding it. We keep following our noses and there it is. Hiding under a black rubber flap at the end of the fish sorting line we find a small collection of fish scales revealed  when the flap is removed for inspection.  With that little section cleaned up and sprayed down the lab is declared done! There is a smile of satisfaction from the team. It is that attention to detail that explains why the lab never smelled of fish when I first boarded the ship 10 days ago nor has it smelled of fish at any time during our voyage. There is a personal pride in leaving the lab in the same shape we found  it. Super clean, all gear and samples stowed, and ready for the next crew to come on board – whenever that turns out to be.

The abrupt and unexpected end to the cruise leaves me scrambling to change my travel plans. Like the ship, I have a limited amount of time to make it home on my government travel orders. The NOAA Teacher at Sea team goes above and beyond to rebook my flights and find me a room for the night.

Personal Log 

On the serendipitous side, the change in plans gives me a little time to see Newport, a town famous for its mansions and the Tennis Hall of Fame.  My first  stop is  the Tennis  Hall  of  Fame.  My father was a first class  tennis  player who invested many  hours  attempting to

teach his  son the game. Despite the passion in  our  home  for  the  great  sport  we  never  made it  to  the  Tennis  Hall  of  Fame in  Newport.  Today I get the  chance to fulfill that  bucket  list  goal. I still remember being court side as a young boy at The  Philadelphia Indoor Championships watching the likes of Charlie Pasarell, Arthur Ashe, and Pancho Gonzales playing on the canvas tennis court that was stretched out over the basketball arena. There was even a picture of the grass court lawn of the Germantown Cricket Club from its days a USTA championship venue before the move to Forest Hill, NY. I grew up playing on those tennis courts as my father belonged to that  club. Good memories.

Clark Log 4b

There was also a  “court tennis” court, the game believed to be the precursor  to outdoor  tennis. Court  tennis derived from playing a  tennis  type  game  inside a walled‐in  court yard.  Using  the  roof and  the  wall and the open side windows to beat your opponent is all part of the game. I played court tennis as a  young teen. It’s a very unique game that is only played in a few spots now. There are only 38 court tennis courts in the world and Newport has two of them. If you like tennis, give court tennis a go if  you ever get the  chance.

The tennis court

Thoughts of a leisurely stroll evolve into a brisk walk as I head toward the ultimate and most famous Newport mansion: The Breakers, the 100,000 plus square foot summer home of the Vanderbilt family. This house has to be toured to understand the conspicuous consumption as a  pastime of the then super rich. My 2000 square foot  home would fit entirely inside  the  grand  hall  of  the  Breakers.  In  fact you could stack my home three high and they would still be below the Breaker’s ceiling. A ceiling inspired by Paris, a billiard room with walls of solid marble overlooking the ocean, a floor of thousands of mosaic floor tiles all put  down by hand one by one, a stair case from Gone With the Wind, and 20 bathrooms to choose from all speak  to the wealth and pursuit of elegance enjoyed by  the Vanderbilt clan. It is a lifestyle of a bye–gone era often referred to as the “Gilded Age.” It is  an apt description.

Clark Log 4dClark Log 4e

Clark Log 4g

After sightseeing, it’s off to the bus stop for my shuttle to the Newport Airport where I take off at dawn the next morning to head for  home. I’m  leaving  so  early that the complementary coffee isn’t out yet! After an uneventful flight comes the end to an amazing adventure. Nothing left now except laundry and memories. And lots of great ideas for lesson plans to work into my classes. Thank you NOAA Teacher at Sea Program for offering me the learning experience of a lifetime. I cannot wait to get back and share the experiences with my students.

Clark Log 4h

John Clark, September 27, 2013

NOAA Teacher at Sea John Clark

Aboard NOAA Ship Henry B. Bigelow

September 23 – October 4, 2013

Clark Log 3gMission: Autumn Bottom Trawl Survey
Geographical Area of Cruise: North Atlantic
Date: September 27, 2013

Science and Technology  Log 

It’s going to be a busy night trawling and processing our catch.  Yippee. I like  being busy as the time passes more quickly and I learn about more fish. A large number of trawling areas are all clustered together for our shift. For the most part that means the time needed to collect data on one trawl is close to the amount of time needed for the ship to reach the next trawling area. The first trawl was a highlight for me as we collected, for the first time,  a few puffer fish and one managed to stay inflated so I had a picture taken with that one.

We found a puffer
We found a puffer

However, on this night there was more than just puffer fish to be photographed with. On this night we caught the big one that didn’t get away. One trawl brings in an amazing catch of 6 very large striped bass and among them is a new record: The largest striped bass ever hauled in by NOAA Fisheries! The crew let me hold it up. It was very heavy and  I kept hoping it would not start flopping around. I could just see myself letting go and watching it slip off the deck and back into the sea. Fortunately, our newly caught prize reacted passively to my photo op. I felt very lucky that the big fish was processed at the station I was working at. When Jakub put the big fish on the scale it was like a game show – special sounds were emitted from our speakers and out came the printed label confirming our prize  – “FREEZ – biggest fish ever “-‐-‐the largest Morone Saxatilis (striped bass) ever caught by a NOAA Fisheries research ship.  It was four feet long. I kept  waiting for the balloons to come down from the ceiling.

Catch of the day
Catch of the day

Every member of the science team sorts fish but at the  data  collection tables my role  in the  fish lab is one of “recorder”. I’m teamed  with  another scientist who serves  as  the “cutter”, in this  case Jakub. That person collects the information I enter into the computer. The amount of data collected  depends on  the quantity and  type of fish  caught in  the net. I help  record  data on length, weight, sex, sexual development, diet, and scales. Sometimes fish specimens or parts of a fish, like the backbone of a goose fish, are preserved. On other occasions, fish, often the small ones are frozen for further study. Not every scientist can make it on to the Bigelow to be directly part of the trip so species data and samples are collected in accordance with their requests.

Collecting data from a fish as large as our striped bass is not easy. It is as big as the processing sink at our data collection  station and it takes Jakub’s skill with a hacksaw-‐-‐yes I said hacksaw-‐-‐to open up the back of the head  of the striped  bass and retrieve  the  otolith, the  two small bones  found behind the head that are  studied to determine  age. When we  were  done, the fish was bagged and placed in the deep freeze for  further  study upon our return. On the good side we only froze one of the six striped bass that we caught so we got to enjoy some great seafood for dinner. The team filleted over 18 pounds of striped bass for the chef to cook up.

Too big for the basket
Too big for the basket

More Going On: 

Processing the  trawl is not the  only data  collection activity taking place on the  Bigelow.  Before most trawls begin the command comes down to “deploy the bongos”. They are actually a pair  of  closed end nets similar to nets used to catch butterflies only much longer. The name bongo comes from the deployment apparatus that holds the pair of nets. The top resembles a set of bongo drums with one net attached to each one. Their purpose, once deployed, is to collect plankton samples for further study. Many fish live off plankton until they are themselves eaten by a predator farther up the food chain so the health of plankton is critical to the success of  the ecological food chain in the oceans.

Processing
Processing

Before some other trawls, comes the command to deploy the CTD device. When submerged to a target  depth  and  running in  the water as the ship  steams forward, this long fire extinguisher sized  device measures conductivity and temperature at specified depths of the ocean. It is another tool for measuring the health of the ocean and how current water conditions can impact the health  of the marine life and also the food chain in the area.

Personal Log 

On a personal note, I filleted a fish for the first time today – a  flounder. Tanya, one  of the science crew taught me how to do it. I was so excited about the outcome that I did another one!

Processing fish
Processing fish

Clark Log 3gg

A mix of fish
A mix of fish
Paired trawl
Paired trawl
Learning to fillet
Learning to fillet

Louise Todd, CTD and Samples, September 25, 2013

NOAA Teacher at Sea
Louise Todd
Aboard NOAA Ship Oregon II
September 13 – 29, 2013

Mission: Shark and Red Snapper Bottom Longline Survey
Geographical Area of Cruise: Gulf of Mexico
Date: September 25, 2013

Weather Data from the Bridge:
Barometric Pressure: 1008.6mb
Sea Temperature: 28.3˚C
Air Temperature: 26.3˚C
Wind speed: 8.73knots

Science and Technology Log:

After we set the line, the CTD (Conductivity, Temperature, Depth) is deployed at each station.

CTD
CTD ready to be deployed

This instrument provides information a complete profile of the physical characteristics of the water column, including salinity, temperature and dissolved oxygen.  The CTD is deployed from the bow of the boat using a winch.

Deploying the CTD
Deploying the CTD

When it is first lowered in the water it calibrates at the surface for three minutes.  After it is calibrated it is lowered into the water until it reaches the bottom.  The CTD records data very quickly and provides valuable information about the station.  Conductivity is used to measure the salinity, the amount of salt dissolved in the water.  The CTD also measures the dissolved oxygen in the water.  Dissolved oxygen is an important reading as it reveals how much oxygen is available in that area.  The amount of oxygen available in the water indicates the amount of life this station could be capable of supporting.  Dissolved oxygen is affected by the temperature and salinity in an area.  Higher salinity and temperature result in lower dissolved oxygen levels.  Areas of very low dissolved oxygen, called hypoxia, result in dead zones.  NOAA monitors hypoxia in the Gulf of Mexico using data from CTDs.

The otoliths and gonads are taken from all of the commercially and recreationally important fish like Snapper, Grouper and Tilefish.  Otoliths are used to age fish.  Aging fish provides information on the population dynamics for those species.  The otoliths are “ear bones” of the fish and are located in their heads.  It takes careful work with a knife and tweezers to remove the otoliths.

Removing otoliths
Removing otoliths

Once the otoliths are removed, they are placed in small envelopes to be examined in the lab in Pascagoula, MS.  Otoliths have rings similar to growth rings in trees that have to be carefully counted under a microscope to determine the age of the fish.

Otolith
Otolith

The gonads (ovaries or testes) are removed and the reproductive stage of the fish is determined.  The weights of the gonads are also recorded.  Small samples of the gonads are taken in order for the histology to be examined in the lab.  Examining the gonads closely will confirm the reproductive stage of the fish.  Gathering information about the reproductive stage of the fish also helps with understanding the population dynamics of a species and aids in management decisions.

Personal Log:

Taking the otoliths out of the fish was harder than I anticipated, especially on the larger fish.  It takes some muscle to get through the bone!

Otolith
Otolith removed from a Red Snapper

We have had a few very busy haul backs today.  One haul back had over 50 sharks!  My favorite shark today was a Bull Shark.  We caught two today but were only able to get one into the cradle long enough to get measurements on it.  We tagged it and then watched her swim away!  I can’t believe we are halfway through my second week.  Time is flying by!  I can’t wait to see what is on the line tomorrow!

Did you Know?

Yellowedge Grouper are protogynous hermaphrodites.  They start their lives as females and transform into males as they age.  Yellowedge Grouper are the only species of grouper we have caught.

Animals Seen

Here are a few of the animals we’ve seen so far!

Tilefish
Tilefish (Photo credit Christine Seither)
Sandbar
Sandbar shark in the cradle
Red Snapper
Red Snapper (Photo credit Christine Seither)
Yellowedge Grouper
Yellowedge Grouper (Photo credit Christine Seither)

John Clark, September 25, 2013

NOAA Teacher at Sea John Clark

Aboard NOAA Ship Henry B. Bigelow

September 23 – October 4, 2013

The galley
The galley

Mission: Autumn Bottom Trawl Survey
Geographical Area of Cruise: North Atlantic
Date: September 25, 2013

Science and Technology  Log 

I was  told  that  the  first  12  hour night watch shift was the hardest for staving off sleep and those who spoke were right. Tonight’s  overnight shift seems to be flying by and I’m certainly awake. Lots of trawling and sorting this  evening with four sorts complete by 6am. One was just full of dogfish, the shark looking fish,  and  they  process  quickly  because  other  than  weight  and  length there is little request for other data. The dogfish were sorted at the bucket end of the job so determining sex had already been completed by the time the fish get to my workstation. Again I’m under the mentorship of Jakub who can process fish faster than I can print and place labels on the storage envelopes. The placement of the labels is my weakness as I have no fingernails and removing the paper backing from the sticky label is awkward and time consuming. Still tonight I’m showing speed improvement over last night. Well at least I’m getting the labels on straight most of the time.

Sorting fish
Sorting fish

In  addition  to  the  dogfish,  we  have  processed  large  quantities  of  skate  (the  one  that  looks  like a  sting  ray to me), left  eyed flounders, croakers (no relation to the frog), and sea robins of which there are two types, northern and stripe. The sea robins are  very colorful with the  array of spines just behind the  mouth. And yes it hurts when one of the spines goes through your glove. Sadly for me sorting has been less exciting tonight.  With  the big fish being grabbed off at the front of the line there has been little left for me to sort. I feel like the goal keeper in soccer  – just  don’t let them get past me. To my great surprise, so far I’ve experienced no real fear of touching the fish. The gloves are very nice to work with.

Species in specific buckets
Species in specific buckets

And let us not overlook the squid. There have been pulled in by the hundreds in the runs today. There are two types of squids, long fin (the lolligo) and short fin (the illex). What they both have in common is the ability to make an incredible mess. They are slimy on the outside and  inky on the inside. They remind me of a fishy candy bar with really big eyes. And  for all the fish  that enjoy their squid  treat the species  is,  of  course,  (wait  for  it) just  eye  candy.  The  stories  about  the  inking  are  really  true. When  upset, they give  off ink; lots of ink. And  they are very upset by the time they reach the data collection stations. If you could bottle their ink you would  never need  to  refill your pen  again. They are also  very, very  plentiful which  might explain  why there are no requests to collect additional data beyond  how long they are. I guess they are not eye candy to marine scientists. However, there vastness is also their virtue. As a food source for many larger species of marine life, an absence of large quantities of squid in our trawling nets would be a bad sign for the marine ecosystem below us.

Safety equipment
Safety equipment

When the squid are missing, our friend the Skate (which of  the four  types does not  matter)  is glad to pick up  the slack on  the “messy to work with” front. As this species makes it down the sorting and data collecting line the internal panic button goes  off and they exude this thick, slimy substance  that covers their bodies and makes them very slippery customers at  the weigh stations.  It turns out the small spines on the tails were placed there so that fisheries researchers could have a fighting chance to handle them without dropping. Still, a skate sliding onto the floor is a frequent event and provides comic relief for all working at the data collection stations.

Clark Log 2There was new species in the  nets tonight, the  Coronet fish which looks like  along  drink straw with stripes  and a string attached to the back end. It is  pencil thick and about a foot long without the string. We only caught it twice during the trip. The rest of the hauls replicate past  sorting as dogfish, robins, skates, squid, croakers, and flounder are the bulk of the catch. I’ve been told that the diversity and size of the trawl should  be more abundant as we steam along the coastline heading north  from the lower coast of  New Jersey. Our last trawl of the shift, the nets deployed collect two species new for our voyage, but ones I actually recognized despite my limited knowledge of fish – the Horseshoe Crab and a lobster! I grew up seeing those on the Jersey shore.  We only got one lobster and after measuring  it we let  go  back  to  grow  some  more.  It  only  weighed in at less than two pounds.

Personal Log 

The foul weather suit we wear to work the line does not leave the staging room where they are stored as wearing them around the ship is not  allowed. After  watching others, I have mastered the art  of  pushing the wader pants over the rubber boots and  thus leaving them set-‐up  for quick donning and  removal of  gear  throughout  the shift.

While the work is very interesting on board, the highlight of each  day is meal time. Even though I work the night  shift (which ends at  noon) I take a nap right after my shift so I can  be  up  and  alert in  time  for dinner. My favorite has been  the T-‐bone steaks with Monterey seasoning and  any of the fish cooked up from our trawling like scallops or flounder. The chef, Dennis, and his assistant, Jeremy serve up some really fine cuisine. Not fancy but very tasty. There is a new soup every day at  lunch and so far my favorite has been the cream of tomato. I went back for seconds! Of course, breakfast is the meal all of us on the night watch  look forward  to  as there is no  meal service between midnight and  7am. After 7 hours of just snacking and  coffee, we are ready for  some solid food by the time breakfast  is served.

Seas continue to be  very calm and the  weather sunny and pleasant. That’s quite a surprise for the North Atlantic in the fall. And  the sunrise today was amazing. The Executive Officer, Chad Cary, shared that the weather we are experiencing should continue for at least four more days. I am  grateful  for  the  calm weather – less  chance  to  experience  sea  sickness.  That is something I’m determined to avoid if possible.

Louise Todd, Haul Back, September 23, 2013

NOAA Teacher at Sea
Louise Todd
Aboard NOAA Ship Oregon II
September 13 – 29, 2013

Mission: Shark and Red Snapper Bottom Longline Survey
Geographical Area of Cruise: Gulf of Mexico
Date: September 23, 2013

Weather Data from the Bridge:
Barometric Pressure: 1009.89mb
Sea Temperature: 28˚C
Air Temperature: 28.2˚C
Wind speed: 8.29knots

Science and Technology Log:

The haul back is definitely the most exciting part of each station.  Bringing the line back in gives you the chance to see what you caught!  Usually there is at least something on the line but my shift has had two totally empty lines which can be pretty disappointing.  An empty line is called a water haul since all you are hauling back is water!

After the line has been in the water for one hour, everyone on the shift assembles on the bow to help with the haul back.  One crew member operates the large winch used to wind the main line back up so it can be reused.

Line on the winch
Winch holding the main line

The crew member operating the winch unhooks each gangion from the main line  and hands it to another crew member.  That crew member passes it to a member of our shift who unhooks the number from the gangion.  The gangions are carefully placed back in the barrels so they are ready for the next station.  When something is on the line, the person handling the gangions will say “Fish on”.

Nurse Shark on the line
Nurse Shark on the line

Everyone gets ready to work when we hear that call.  Every fish that comes on board is measured. Usually fish are measured on their sides as that makes it easy to read the markings on the measuring board.

Measuring Grouper
Measuring a Yellowedge Grouper (Photo credit Christine Seither)
Measuring a Sandbar
Christine and Nick measuring a Sandbar Shark

Each shark is examined to determine its gender.

Sexing a shark
Determining the sex of a sharpnose shark (Photo credit Deb Zimmerman)

Male sharks have claspers, modified pelvic fins that are used during reproduction.  Female sharks do not have claspers.

Claspers
Claspers on a Blacktip

Fin clips, small pieces of the fin, are taken from all species of sharks.  The fin clips are used to examine the genetics of the sharks for confirmation of identification and population structure, both of which are important for management decisions. 

Shark Fin Clip
That’s me in the blue hardhat taking a fin clip from a Sandbar Shark(Photo credit Lisa Jones)

Skin biopsies are taken from any dogfish sharks  in order to differentiate between the species.  Tags are applied to all sharks. Tags are useful in tracing the movement of sharks.  When a shark, or any fish with a tag, is recaptured there is a phone number on the tag to call and report the location where the shark was recaptured.

Some sharks are small and relatively easy to handle.

Cuban Dogfish
Small Cuban Dogfish (Photo credit Christine Seither)

Other sharks are large and need to be hauled out of the water using the cradle.  The cradle enables the larger sharks to be processed quickly and then returned to the water.  A scale on the cradle provides a weight on the shark.  Today was the first time my shift caught anything big enough to need the cradle.  We used the cradle today for one Sandbar and two Silky Sharks.  Everyone on deck has to put a hardhat on when the cradle is used since the cradle is operated using a crane.

Silky Shark
Silky shark coming up in the cradle
Sandbar Shark
Sandbar Shark in the cradle

Personal Log:

I continue to have such a good time on the Oregon II.  My shift has had some successful stations which is always exciting.  We have had less downtime in between our stations than we did the first few days so we are usually able to do more than one station in our shifts.  The weather in the Gulf forced us to make a few small detours and gave us some rain yesterday but otherwise the seas have been calm and the weather has been beautiful.  It is hard to believe my first week is already over.  I am hopeful that we will continue our good luck with the stations this week!  The rocking of the boat makes it very easy for me to sleep at night when my shift is over.  I sleep very soundly!  The food in the galley is delicious and there are plenty of options at each meal.  I feel right at home on the Oregon II!

Did You Know?

Flying fish are active around the boat, especially when the spotlights are on during a haul back at night.  Flying fish are able to “fly” using their modified pectoral fins that they spread out.  This flying fish flew right onto the boat!

FlyingFish
Flying Fish

John Clark, Hi Ho, Hi Ho It’s Off to Work We Go, September 24, 2013

NOAA Teacher at Sea
John Clark
Aboard NOAA Ship Henry B. Bigelow
September 23 – October 4, 2013

Mission: Autumn Bottom Trawl Survey
Geographical Area of Cruise: North Atlantic
Date: September 24, 2013

Survival suits!
Survival suits!

Science and Technology  Log 

Today is my first full 12 hour shift day. I’m on the night crew working midnight to noon. Since we left port yesterday I’ve been  trying to  adjust my internal clock for pulling daily “all night”ers.  On Monday, after we  left port, safety briefs for all hands occurred once we made it out to sea and I got to complete my initiation into the Teacher at Sea alumni program  – the donning of  the Gumby suit as I call it. It is actually a bright red wet suit that covers your entire body and makes you look like a TV Claymation figure from the old TV show. In actuality it is designed to help you survive if  you need to abandon ship. Pictures are  of course taken to preserve this rite of passage.

The Henry B. Bigelow is a specially-built NOAA vessel designed to conduct fisheries research at sea.  Its purpose is to collect data that will help scientists assess the health of the Northern Coastal Atlantic Ocean and the fish populations that inhabit it. The work is invaluable to the commercial fishing industry.

The Bigelow in port
The Bigelow in port

Yesterday, I learned how we will go about collecting fisheries data. Our Chief Scientist, Dr. Peter Chase, has selected  locations for sampling the local fish population and the ship officers have developed a sailing plan that will enable the ship to visit all those locations, weather permitting, during the course of the voyage. To me its sounds like a well-‐planned  game of connecting the dots. At each target location, a trawling net  will be deployed and dragged near the bottom of the sea for a 20 minute period at a speed of 3 knots. Hence the reason  this voyage is identified as a bottom trawl survey mission. To drag the bottom without damaging the nets is not easy and there are five spare nets on board in case something goes wrong. To minimize the chance of damaging the net during a tow, the survey technicians use the wide beam sonar equipment to survey the bottom prior to deployment. Their goal is to identify a smooth path for the net to follow. The fish collected in the net are sorted and studied, based on selected criteria, once on board. A  specially designed transport system moves the fish from the net to the sorting and data collection stations inside the wet lab. I’m very excited to see how it actually works during my upcoming shift.

The big net.
The big net.

Work is already underway when our night crew checks in. The ship runs 24/7  and the nets have been down  and trawling since 7pm. Fish sorting and data collection  are  already underway.  I don my foul  weather gear which  looks  like a set of waders used for British fly fishing.  There is also a top jacket  but the weather is pleasant  tonight and the layer is not needed. I just need to sport some gloves and get to work. I’m involved with processing  two trawls of fish right away. I’m assigned to work with an experienced member of the science team, Jakub. We will be collecting information on the species of fish caught on each trawl.  Jakub carries out the role as cutter, collecting the physical  information or fish parts needed by the scientists. My role is recorder and  I enter data about the particular fish  being evaluated  as well package up  and  store the parts of the fish  being retained  for future study.

Ship equipment
Ship equipment

Data collection on each fish harvest is a very detailed. Fish are sorted by species as they come down the moving sorting line where they arrive after coming up the conveyer belt system from the “dump”  tank, so  named  because that is where the full nets deposit their  bounty. Everybody on the line sorts fish. Big fish get  pulled off  first  by the experienced scientists at  the start  of  belt  and then volunteers such as I pull off the smaller fish. Each  fish  is placed  into  a bucket by type of fish. There are three types of buckets and each bucket has a  bar code  tag. The  big laundry  looking  baskets  hold  the  big  fish,  five  gallon  paint buckets hold  the smaller fish, and  one gallon  buckets (placed  above the sorting line) hold  the unexpected  or small species. On  each  run  there is generally one fish  that is not sorted  and  goes all the way to the end untouched and unceremoniously ends up in the catch-‐all container at the  end of the  line. The watch leader weighs the buckets and then links the bar code on the bucket to the type of fish in it. From there  the  buckets are  ready for data  collection.

Clark Log 1d
The sorting line

After sorting the fish, individual data collection begins “by the bucket” where simultaneously at three different stations the sizing, weighing, and computer requested activities  occur. By  random sample certain work  is  performed on that fish. It  gets weighed and usually opened up to retrieve something from inside the fish. Today, I’ve observed several types of  data collection. Frequently requested are removal of  the otolith, two small bones in the head that  are used to help determine the age of  the fish. For bigger fish with vertebra,  such  as  the  goose  fish,  there  are periodic  requests  to  remove a  part  of  the backbone and  ship  it off for testing. Determining sex is recorded  for many computer tagged  fish  and  several are checked stomach contents.

Of the tools used to record data from the fish, the magic magnetized measuring system is the neatest. It’s  rapid  fire  data  collecting  at  its  finest.  The  fish  goes  flat  on  the measuring  board;  head  at  the  zero point, and  then a quick touch  with  a magnetized block at the end  of the fish  records the length  and  weight. Sadly, it marks the end of tall tales about the big  one that got  away and keeps getting bigger as the story is retold. The length of  the specimen is accurately recorded for  posterity in an instant.

 

clark 1e

Personal Log

Flying into Providence  over the  end of Long Island and the  New England coast line  is breath taking. A jagged,  sandy  coast  line  dotted  with  summer  homes  just  beyond  the  sand dunes. To line  up  for  final  approach we  fly right over Newport where  the  Henry B. Bigelow is berthed at the  Navy base  there. However, I  am  not  able  to  spot  the  NOAA  fisheries  vessel that  will be my home for the next two weeks from the air.Clark Log 4b

I arrive a day prior  to sailing so I have half a day to see the sites of Newport, Rhode Island  and  I know exactly where  I’m headed – the Tennis Hall of  Fame. My father was a first class tennis player who invested  many  hours  attempting  to  teach  his  son  the  game.  Despite  the  passion in  our  home  for  the great sport we  never made  it to the  Tennis Hall of Fame in Newport. Today I fulfilled that bucket  list  goal. I still remember being  court side  as a  young boy at The  Philadelphia  Indoor Championship watching the likes of  Charlie Pasarell, Arthur  Ashe, and Pancho Gonzales playing  on the canvas tennis court that was stretched out over the basketball arena. Also  in  the museum, to  my surprise, was a picture of the grass court lawn of the  Germantown Cricket Club from its days as a USTA championship venue. I  grew up playing on  those  grass tennis courts as my father  belonged to that  club. After seeing that picture, I left the museum knowing my father  got  as much out  of  the visit  as I did.

Susy Ellison, Aaargh Matey, How’s Your Number Sense? September 22, 2013

NOAA Teacher at Sea
Susy Ellison
Aboard NOAA Ship Rainier
September 9-26, 2013 

Mission:  Hydrographic Survey
Geographic Area:  Cold Bay, Alaska
Date:  September 22, 2013   

Weather:  current conditions from the bridge
GPS Location: 55o 15.190’ N   162o 38.035’ W
Temp: 8.6C
Wind Speed: 10 kts
Barometer: 1008.3mb
Visibility: 10 miles

You can also go to NOAA’s Shiptracker (http://shiptracker.noaa.gov/) to see where we are and what weather conditions we are experiencing.

If you want a detailed report of weather in our area, check out this link and hover over Cold Bay: http://pafc.arh.noaa.gov/index.php?index=bering   

Science and Technology Log

THE FINE ART OF STARING AT A STICK!

Why am I sitting here?  What am I looking at?
Why am I sitting here? What’s out there?

 What would you think if you saw someone bundled in warm clothing, sitting in an office chair on a pier with a pair of binoculars, a watch, and a clipboard?  Are they counting waves? Counting birds?  Keeping track of the clouds or the wind speed?  In my case it was ‘none of the above’; I was watching a measuring stick, taking measurements every 6 minutes over a period of 3 hours.  Why would anyone want to sit in a chair on a pier and stare at a stick for 3 hours?

The answer, of course, is science! Now, this wasn’t just any sort of stick.  This tide staff was attached to an automatic tide gauge that the crew of the Rainier installed during their last visit to Cold Bay in August.  That gauge has been recording tidal data that is used during their hydrographic survey work.  But, as with any automatic data-gathering device, it is critical to field check its accuracy, both in measuring and reporting the data.  The gauge measures the depth of the water column at 6-minute intervals, using the pressure of the water column as a proxy for that depth (deeper water exerts a greater pressure on the subsurface opening of the gauge—for a more in-depth explanation, you can check out my blog from September 13th).  My job was to stare at the staff for a period of 1 minute every 6 minutes, and determine both the highest and lowest height of the water lapping at the markings on the stick.

This might sound easy, but it wasn’t quite so simple.  The wind was howling and the waves were bouncing—it took a little practice to make what I hoped was an accurate estimate of both the high mark and the low.  After each observation period I recorded these numbers on a spreadsheet and then spent the next few minutes watching the birds that were flying and landing on the water.  Then—back to the stick!  The tide was dropping with each observation and the winds died down enough to make it a little easier to read the high and low points on each successive 6 minute interval.  By the 10th observation I had it figured out!

NOAA Corps ENS Clark demonstrates proper form for tide gauge observation.
NOAA Corps ENS Clark demonstrates proper form for tide gauge observation.
Picture trying to read this from far away as the water bounces up and down the staff.
Picture trying to read this from far away as the water bounces up and down the staff.

The data I collected was matched against data from the tide gauge for that same time period.  I was pleased to see that my observations matched those of the gauge.  Apparently, both of ‘us’ are good observers of tidal changes.  Now I have one more skill to add to my resume!!

This graph compares my observations with that of the tide gauge.  What do we observe vs. what does a computer measure?
This graph compares my observations with that of the tide gauge. What do we observe vs. what does a computer measure?

AAARGH, MATEY—HOW’S YOUR NUMBER SENSE?   APPLIED MATH ON THE HIGH SEAS  

It would be hard to find an aspect of life aboard the Rainier that doesn’t involve number sense or math.  This ship’s daily operations run like clockwork; breakfast from 0700-0800, Safety Meeting and deployment of the launches at 0800, lunch from 1130 to 1230, launches return at 1630, dinner from 1700 to 1800, etc.  Pretty simple numbers to deal with, but numbers, nonetheless.

That’s just the start of your applied math tour of the high seas. Maybe you have to figure out how much diesel fuel the ship has onboard.  Since the Rainier uses 20,000-40,000 gallons for each leg of its cruise, it would be pretty horrible to run out before you reached port.  The ship’s tanks can hold around 100,000 gallons of diesel and are usually filled to within 95% of that.  Unlike your car, there’s no fuel gauge on this ship.  So how do you figure out how much fuel is in the tank?  It’s time for some simple, yet essential math. First, you need to know the volume of the fuel tank.   Get out your math books and find that formula.  Then, you take what is called a ‘sounding’—you bang on the tank to determine the level of fuel.  Not too complicated, but certainly a skill that takes some practice.  So, now you know the total volume of the tank as well as the actual height of your fuel; if you figure out the volumes for each and do some subtraction, you can find out what percentage of your total fuel is still in the tank.

We might all be better at determining volume and percent if we had images of a fuel tank on the dashboards of our cars instead of a linear gauge reading ‘E’ to ‘F’! What about drinking water?  The Rainier uses a distillation system to create fresh water from seawater.  There are tanks down in the engine room where seawater is heated to the boiling point.  There’s a little more math and science in this process—the pressure in the distillation tank is lowered, to lower the boiling point (if you’ve ever camped at a high elevation you might notice that water boils at a lower temperature—your tea might not be quite as hot when it’s boiling) so the water doesn’t have to be heated quite so much to get it to boil.  This steam is captured in the upper portion of the distiller and cooled using cold seawater that flows through pipes.  The condensation from cooling is captured, filtered to remove any impurities, and distributed as fresh water to all onboard.  The ship uses around 2500 gallons of water each day.

Here's where all our fresh water is produced.  This distiller takes in seawater and, through boiling and condensation, produces fresh water.
Here’s where all our fresh water is produced. This distiller takes in seawater and, through boiling and condensation, produces fresh water.

If you’re running the galley it’s essential to calculate how much food you’ll need for each leg of the trip.  No one wants to do without their morning eggs if your multiplication is off and you ‘forget’ to buy a few dozen.  Taking a recipe that is designed to feed 8 people and ‘upsizing’ it for 48 people takes a bit of mathematical manipulation.  Just planning a menu for a three-week journey takes some mathematical thinking as you visualize the weeks, days, meals, and individual ingredients needed for those meals.  You have to factor in a few variables; which foods have the longest shelf life, when do you have to switch from fresh to frozen or to canned foods, how much food does the ‘average’ person eat, and what about all those people with food allergies or preferences?  While this might not sound quite as earth-shattering as using a detailed computer program to concatenate multiple data files, this is math that counts—especially when you’re feeding a boatload of hungry crew.

This is a glimpse of some of the supplies stored on the ship.
This is a glimpse of some of the supplies stored on the ship.
Don't forget to buy enough fruit and vegies!
Don’t forget to buy enough fruit and vegies!
Hmmm, what's in the freezer?
Hmmm, what’s in the freezer?

So now it’s time to consider the math used to pilot the ship.  Think about degrees in a compass bearing and the need to do some rapid mental math as you’re steering a 231-foot ship through some very tight spaces.  Quick—take a course of 340o, now look ahead and get ready to change your bearing to 28oRainier’s draft (how deep it sits in the water) is around 16’.  Will the channel be deep enough?  What if you’re traveling in a supertanker, one that might be over 400’ in diameter and have a draft up to 80’ deep?  If your ship is that big, you need to scale up on your mental math calculations as you’re searching out appropriate harbors and routes! What about tying up the ship when we’re in harbor? Did you remember to learn something about vectors before you stopped taking math classes?

When we were at port in Cold Bay, the winds were expected to increase in strength and to shift so that they would be coming out of the west.  Since the pier was oriented perpendicular to the predicted wind direction, our Chief Bo’ sun, Jim Kruger had to do some mental calculations of the angles needed to secure the ship to the pier and keep it from bouncing too much.  He doubled and even tripled some of the lines, taking into account how the winds might move the ship as well as the strength of each line.  It takes some stout lines to hold this ship; each 300 ft. line is 1” in diameter and has a tensile (breaking) strength of 164,000 lbs.    Vector angles were equally important as we pulled away from the pier in a 50-knot wind.  Just pulling up our gangway with a crane required some careful mental calculations of where to place lines to steady it as it rose through the air and was lifted onboard. If your mental math and visualization skills were wrong, you might be rewarded with a wildly swinging piece of metal.

Double (and triple) up the lines holding the ship to the pier.  Make sure the angles are right.
Double (and triple) up the lines holding the ship to the pier. Make sure the angles are right.
Hang tight to the gangway as it swings onboard.  Make sure you're holding it at the correct angle to compensate for the wind.
Hang tight to the gangway as it swings onboard. Make sure you’re holding it at the correct angle to compensate for the wind.
Strong winds--this digital anemometer records current wind speed in knots as well as the highest gust.
Strong winds–this digital anemometer records current wind speed in knots as well as the highest gust.

How about all that hydrographic data collection; there’s plenty of opportunity there for some pretty extreme mathematical calculations.  You might even wish you had taken a class in calculus—or a few classes!  But there are also plenty of times that some basic number sense and arithmetic come in mighty handy.  As I sat on the pier watching the tide gauge, one of the tasks I had to do was to calculate the average between high and low water marks on the tide staff.  Not such hard math, but it’s a good skill to be able to do averages in your head while your hands are getting cold and the wind is howling.  The tide gauge calculations were referenced to Coordinated Universal Time (UTC). This has been our world standard since 1972, and is referenced to the 0o meridian at Greenwich, England.  It is precisely measured using an atomic clock.  You might also hear it referred to as Zulu Time.  Even airplanes use this time designation.  This way, there is no ambiguity about whether you are in daylight savings or standard time, or your time zone.  When measuring tides or collecting information about water chemistry using the CTD, or calculating the launch’s daily gyrations, it is important to reference everything to the same time standard.  Since the Rainier is on RST (Rainier Standard Time), the calculation gets even more important because we are in the Alaska time zone, but have set our clocks back one more hour to give us more daylight working hours).

What's your time zone?  GMT stands for Greenwich Mean Time.  It is also the UTC time standard we use.
What’s your time zone? GMT stands for Greenwich Mean Time. It is also the UTC time standard we use.

Just in case your brain hasn’t been addled by all this talk of mathematics, there’s one more concept that might come in handy here on the high seas—a sine wave.  Huh?  Sine waves are a mathematical curve describing smooth repetitive oscillations.  Like…tides, sonar pulses, sunrise/sunset observations, or the music booming out of your iPod.

Tide charts show a predictable, repeatable sine wave pattern.
Tide charts show a predictable, repeatable sine wave pattern.

I even use math to calculate how long I should run on the elliptical trainer down in the ship’s exercise space.  If I set the resistance to 8, and use a cross training setting, it takes around 35 minutes to ‘run’ the equivalent of one slice of cake!

Here's some of the exercise equipment on the ship.
Here’s some of the exercise equipment on the ship.
35 minutes or one slice of pie--whichever comes first!
35 minutes or one slice of pie–whichever comes first!

Just in case you haven’t gotten the message—math is good.  Number sense is critical—even if you want to run off to sea!

Personal Log

IT’S A FIELD TRIP!!

The entire Cold Bay School fits into this truck!
The entire Cold Bay School fits into this truck!

I love a field trip.  There’s nothing like loading up in the bus and taking off in search of the great unknown.  While we were parked at the Cold Bay pier, we had a visit from the Cold Bay School.  The 8 students, plus their teacher and a classroom aide, came to check out the Rainier.  CO Rick Brennan gave them a tour, starting at the bridge, and ending with lunch in the wardroom.  Along the way, they learned about ships and ship life, NOAA, and the science of hydrography. Lunch was a real hit, since the kids all bring their own lunches to school.  Who wouldn’t like halibut tacos with all the fixings from the galley, or a peanut butter and jelly sandwich handmade by Commander Rick Brennan with a fresh cookie for dessert?

Cold Bay students check out some of the ship's BIG tools.
Cold Bay students check out some of the ship’s BIG tools.

I tagged along on the tour to talk with some of the kids and their teacher and to compare notes about schools.  While I always think of my school as small, with only 150 students, the school in Cold Bay is really small.  There are 8 students and they represent grades 1 through 7.  While the school is small, each student uses an iPad to access a wide variety of educational resources. It’s even better when that technology-based learning is supplemented by some hands-on field trip-based learning.  This was their second field trip of the week; they had spent a day with a wildlife biologist helping install a motion-sensitive camera in the Izembek Wildlife Refuge (http://www.fws.gov/alaska/nwr/izembek/index.htm).

Future hydrographers head back to school.
Future hydrographers head back to school.

SAFETY FIRST

Where I live, in Colorado, we occasionally get snow days, when the roads are too dangerous to transport children to school.  Here at sea, we don’t worry too much about snow, but wind can create hazardous working conditions.  Yesterday we had what I would call a ‘Wind Day’; none of the survey launches went out.  The winds were gusting up to 50 knots, and were fairly steady at 30 knots.  That’s windy.  The surface of the bay was a froth of water, waves, and whitecaps.  Even the Black-legged Kittiwakes were having trouble flying!

Whitecaps all across the bay.  Definitely NOT a day to survey the sea floor.
Whitecaps all across the bay. Definitely NOT a day to survey the sea floor.

Certainly not the sort of day where you want to send out teams of hydrographers in 28 foot long launches.  While safety is paramount, data quality also suffers in such ‘bouncy’ seas.  As the launch bounces from side to side or from front to back, the sonar sends its pings far afield.  It becomes difficult or impossible to drive straight, overlapping lines as you ‘mow the lawn’ through your polygon (Wait, there’s another math term!) , and turning the craft requires timing and skill as you move through the rolling seas.  As the Rainier nears the end of its time at sea and in Cold Bay, each day becomes critical to achieve its charting goals—but there’s plenty of work to do on board on a day like this.  

   

Susy Ellison, From Dragons to Data – Mapping Our World, September 18, 2013

NOAA Teacher at Sea
Susy Ellison
Aboard NOAA Ship Rainier
September 9-26, 2013

Mission:  Hydrographic Survey
Geographic Area: South Alaska Peninsula and Shumagin Islands
Date:  September 18, 2013

Weather:  current conditions from the bridge

You can also go the NOAA’s Shiptracker (http://shiptracker.noaa.gov/) to see where we are and what weather conditions we are experiencing.

GPS coordinates: 55o  12.442’ N  162o 41.735’ W
Temp:  9.6C
Wind Speed:  20.3 kts
Barometer: 994.01mb
Visibility:  grey skies, foggy

Science and Technology Log

WHERE ARE WE? HOW DO WE KNOW?

As we float about all day collecting gigabytes of data to turn into charts, there’s ample time to reflect on the art and science of cartography, or map making.  To me, maps are an elegant means for transforming the 3-dimensional landscape around us into a 2-dimensional story of our world using lines and points, geometric shapes, numbers, and a variety of colors and shadings.  It’s science, technology, engineering, math, and, as always, a bit of magic! It’s quite amazing to think about the changes in mapmaking and our expectations for information from the first hand-drawn lines on small pieces of clay or in the dirt to the concatenated gigabytes of today.

Consider some of the earliest maps that have been found.  Archaeologists have unearthed clay tablets in Babylonia that date back to 600 BC.  These hand-sized clay tablets were simple line representations of local geography.  Roman maps from around 350BC were utilized to provide information to conquering armies.  Where were they heading; which villages were going to be conquered today?

This is one of the earliest known maps.  It is a clay tablet from Babylonia. http://www.britishmuseum.org/explore/highlights/highlight_objects/me/m/map_of_the_world.aspx
This is one of the earliest known maps. It is a clay tablet from Babylonia.
2peutinger map
Romans used maps to identify villages and towns along the routes of conquering armies.
http://www.datavis.ca/milestones/index.php?group=pre-1600
3paleolithic map
Here’s an early map drawn on stone.

The earliest maps were, both literally and figuratively, flat;  they were a 2 dimensional image of a world that was believed to be flat.  That changed in 240 BC when Eratosthenes, who believed the earth to be a sphere, calculated earth’s diameter by comparing the length of noontime shadows at distant sites.  No advanced computing power was used for this calculation!  Once geographers and cartographers were united in their use of a spherical representation of the earth, the next challenge was how to project that spherical surface onto a flat page.  Ptolemy, sometime around 100 AD figured this out.  He went a step further, assigning grid coordinates (latitude and longitude) to the maps to use as identifiers.  His latitude lines, rather than expressed as degrees from the equator, were categorized by the length of the longest day—not such a bad proxy for degrees north and south and certainly an obvious change as you head north or south.  Longitude, instead of referencing the Greenwich Meridian as 0o, was set at 0 at the westernmost point that he knew.  Much of his work was not used until it was rediscovered by monks poring through manuscripts in the 1300s.  One monk was able to use the coordinates in these manuscripts to create graphic representations (maps!) of Ptolemy’s concepts.  These were printed in 1477 as a map collection known as Geographia.  It is almost mind-boggling to consider the efforts that went into this volume from its initial intellectual conception, to its rediscovery, to using some of the first printing presses to make multiple copies that were used to plan and guide some of our most amazing voyages of discovery.  Ptolemy’s concepts were further refined when Gerardus Mercator  invented a cylindrical projection representing globe on a map’s flat surface.  Each refinement both changed and enhanced our view of the planet.

Mercator solved the challenge of projecting a round earth onto a flat surface http://upload.wikimedia.org/wikipedia/commons/5/58/Mercator_World_Map.jpg
Mercator solved the challenge of projecting a round earth onto a flat surface
http://upload.wikimedia.org/wikipedia/commons/5/58/Mercator_World_Map.jpg

 THERE MAY BE DRAGONS

Sailors set forth with maps using these concepts for many years, seeking out new lands and new wealth for the countries they represented.  As they returned with new discoveries of continents, cultures, and meteorological conditions, they were able to replace some of the ‘dragons’ on maps with real information and add new layers of information on top of the positions of continents and oceans—an early sort of GIS (geographic information systems) process!  In 1686, Edmond Halley created a map that incorporated the prevailing winds atop a geographical map of the world.  A new layer of information that told a critical story.  For a sailor navigating using the wind, the story this map told was incredibly useful.   Further layers were placed on the surface geography as Johann Friedrich von Carpenter created the first geological map in 1778.  This map included information about what was under the surface, including soils and minerals.

Halley's map included information about global wind patterns.  Pretty important if you're on a sailboat navigating around the world!
Halley’s map included information about global wind patterns. Pretty important if you’re on a sailboat navigating around the world!
The first geological map included information about what lay below the surface http://earthobservatory.nasa.gov/IOTD/view.php?id=8733
The first geological map included information about what lay below the surface
http://earthobservatory.nasa.gov/IOTD/view.php?id=8733

To me, perhaps one of the fundamental changes in how we represented the earth came in 1782, when the first topographic map was created.  Marcellin du Carla-Boniface added still more layers of information to our ‘flat’ surface, including contour lines that were like slices of the landscape whose spacing indicated the slope of the feature.  Suddenly, we were going from a 3-dimensional world, to a 2-dimensional image, and back to a system of symbols to represent that third dimension.  More data, more layers, more information on that one sheet held in your hand, and a more detailed ‘story’ of the landscape.  Each cartographical and technological advance has enabled us to put more information, with increasing accuracy, upon our maps.  Go one step further with this and click on Google Earth.  A 3-dimensional view on a 2-dimensional screen of 3-dimensional data. Go one more step as you use your smartphone to display a 2-dimensional image taken from a 3-dimensional Google Earth view, made using layers of information applied to a flat map image.  It’s a bit more sophisticated than the original flat clay tablet—but it basically ‘tells’ you how to get from here to there. While the complexity of our world has not actually increased, the stories we are telling about our planet have increased exponentially, as has our ability for combining datum from a variety of sources into one, tidy little package.

This is a small piece of the first topographic map which included elevation information about surface features http://www.datavis.ca/milestones/

This is a small piece of the first topographic map which included elevation information about surface features
http://www.datavis.ca/milestones/

A modern topographjic map, produced by USGS
A modern topographjic map, produced by USGS

THERE MAY BE DATA!

With each new technique and layer of information our ability to tell detailed stories with maps has improved.  We can add data to our maps using colors—just look at a modern colorful weather map in USA Today if you want to see an example of this.  Early cartographers used colors and shading to depict disease outbreaks or population numbers.  Here on the Rainier, we use color variations to show relative depth as we survey the ocean floor. The final charts have lines to denote depth changes, just as lines on a land-based topographic map show changes in elevation.

So, you might be asking yourself at this point, ‘How does a history of mapping relate to mapping the coastline in SW Alaska?’ Why are we currently anchored out here near Cold Bay, Alaska?  NOAA had its beginnings in 1807 when the first scientific agency, the Survey of the Coast, was established.  Since then, NOAA’s mission has broadened to include the following “NOAA is an agency that enriches life through science. Our reach goes from the surface of the sun to the depths of the ocean floor as we work to keep citizens informed of the changing environment around them.”  We are here as part of that mission, working through their National Ocean Service.   You might not realize it, but almost every imported item you buy spent some part of its life on a ship.  While Alaska’s coastline may seem a trifle remote, if you check out a map you might notice that it’s almost a straight shot from some of the ports in Asia to the west coast of the US.

Nautical chart showing the Cold Bay area
Nautical chart showing the Cold Bay area
A Google Earth image of Cold Bay
A Google Earth image of Cold Bay
Take a look at this map of the major world shipping routes.  See how many pass near SW Alaska.
Take a look at this map of the major world shipping routes. See how many pass near SW Alaska.

The Alaska Maritime Ferry also passes through these coastal areas on its way to towns and villages.  While these areas are, indeed, remote, they are united by a common coastline.  The Rainier, in over 40 years of ‘pinging’ its way northward each season from Washington and Oregon, has mapped this coastline.  That, to me, is an amazing feat!

Think of where we’ve come in our ability to tell stories about our landscape and how the intersection of all those stories has played a part in creating the world in which we live.  I, for one, still delight in the most simple of maps, drawn on a scrap of paper or the back of a napkin, showing someone how to get from point ‘a’ to point ‘b’.  Those maps are personal, and include the layers of information that I think are important (turn left at this house, turn right at that hill, go 2 miles, etc) and that tell the story I want to tell.  We now have the ability to add endless layers to our mapping stories, concatenating ever more data to tell an amazingly precise version.  In spite of this sophistication I hope there’s still a few dragons left out there!

There still may be some dragons out there!!
There still may be some dragons out there!!

If you want to know more, here’s some of the websites I looked at while researching this information:

http://oceanservice.noaa.gov/navigation/hydro/#1

http://www.noaa.gov/

http://www.nesdis.noaa.gov/

http://specialprojects.nos.noaa.gov/welcome.html

http://www.datavis.ca/milestones/index.php?page=introduction

 For a great cartographic mystery, check out this book:

The Island of Lost Maps;  A True Cartographic Crime by Miles Harvey

Personal Log

Today’s blog blends the scientific with the personal.  Maps are both of these things; a way to categorize and document our planet in a methodical, reasoned, repeatable, and scientific manner, and a way to personalize our planet to tell a story that we want to tell.  Cool stuff to think about as we drive back and forth across our little polygon here in Cold Bay.  It puts our work into perspective and creates both a sense of its importance and its relevance to describing a piece of our planet.  Hmmmm, in my next lifetime maybe I should be a hydrographer……

Student Driver!
Student Driver!
driving 2
I might need to fine tune my driving skills before anyone really lets me be a hydrographer. Those white gaps are ‘holidays’–no data was collected. 

Louise Todd, Setting the Line, September 19, 2013

NOAA Teacher at Sea
Louise Todd
Aboard NOAA Ship Oregon II
September 13 – 29, 2013

Mission: Shark and Red Snapper Bottom Longline Survey
Geographical Area of Cruise: Gulf of Mexico
Date: September 19, 2013

Weather Data from the Bridge:
Barometric Pressure: 1017.17mb
Sea Temperature: 28.8˚C
Air Temperature: 27˚C
Wind speed: 18.05 knots

Science and Technology Log:

Those of you following our progress on the NOAA Ship Tracker might have noticed some interesting movements of the ship.  We had some rough weather that forced us to skip a station, and the current by the mouth of the Mississippi River also forced us to skip a station.  The safety of everyone on board comes first so if the seas are too rough or the weather is bad we will skip a scheduled station and move to the next one.  Now we are off the coast of Florida and hope we can get some good fishing done!

This survey is being done using longlines.  Longlines are exactly as their name describes, long stretches of line with lots of hooks on them.  The line we are using is 6,000 feet long, the length of one nautical mile.  From that long line, there are 100 shorter lines called gangions hanging down with hooks on the end.  Each gangion is 12 feet long.

Gangions
Gangions in the barrel

When we arrive at a sampling station, everyone on our shift helps to set the line.  In order to set the line, we have to bait each one of the hooks with mackerel.

Baited gangions
Baited gangions ready to go

Once the hooks are baited, we wait for the Officer of the Deck (OOD), driving the ship from the bridge, to let us know that we are in position at the station and ready to start setting the line.  The first item deployed is a high flyer to announce the position of our line to other boats and to help us keep track of our line.

High Flyers
High flyers ready to be deployed

This is a bottom longline survey so after the high flyer is deployed, the first weight is deployed to help pull the line to the bottom of the ocean just above the seabed.  After the first weight is deployed, it is time to put out the first 50 hooks.  This is typically a three person job.  One person slings the bait by pulling the gangion from the barrel and getting ready to pass it to the crew member.  Another person adds a number tag to the gangion so each hook has its own number.

Numbers for hooks
Number clips are attached to each gangion

A member of the deck crew attaches each gangion to the main line and sends it over the side into the water.  The gangions are placed 60 feet apart.  The crew members are able to space them out just by sight!  The bridge announces every tenth of a mile over the radio so they are able to double check themselves as they set the line.  Another weight is deployed after the first 50 hooks.  A final weight is placed after the last hook.  The end of the line is marked with another high flyer.  Once the line has been set, we scrub the gangion barrels and the deck.  The line stays in the water for one hour.

Once the line has soaked for one hour, the fun begins!  Haul back is definitely my favorite part!  Sometimes it can be disappointing, like last night when there was absolutely nothing on the line.  Other times we are kept busy trying to work up everything on the line.  When the line is set and brought back in, everything is kept track of on a computer.  The computer allows us to record the time and exact location that every part of the line was deployed or retrieved.  The touchscreen makes it easy to record the data on the computer.

Computer
Computer ready to document what is on each hook

Personal Log:

It is nice to be doing some fishing!  There have been some long distances in between our stations so my shift has not gotten the opportunity to set the line as much as we would like.  I’m hopeful that the weather holds out for us so we can get a few stations in on our shift today.  Being able to see these sharks up close has been amazing.  I am enjoying working with the people on my shift and learning from each one of them.  Before we haul back the line, I ask everyone what their guess is for number of fish on the line.  My number has been 45 the past few haul backs and I’ve been wrong every time!  Christine was exactly right on one of our last haul backs when she guessed two.  I know I’ll be right one of these stations.  It is hard to get pictures of what comes up on the line because we get so busy processing everything.  I’m going to try to get more pictures of our next stations.

The views out in the Gulf are gorgeous.  I never get tired of them!

Moon Rising
Can you see the moon?
Sunset over the Gulf
Sunset over the Gulf

Did You Know?

When we arrive at a sampling station, the officer on watch must be aware of other ships and rigs in the area.  At times the bridge watchstander will make the decision to adjust the location of our sampling station based on large ships or rigs in the area.

Rig and Ship
Rigs and other ships in the area of a sampling station can force us to move the station

John Clark, To the Henry B. Bigelow – Bound and Determined, September 18, 2013

NOAA Teacher at Sea
John Clark
Aboard NOAA Ship Henry B. Bigelow
September 23 – October 4, 2013

Mission: Autumn Bottom Trawl Survey
Geographical Area of Cruise: North Atlantic
Date: September 18, 2013

Introduction

Thank you for reading about my adventures at sea. My name is John Clark and I’m entering my 7th year teaching science at Deltona High School in Deltona, Florida. Our community is just off I-4 between Orlando and Daytona Beach. Teaching is my second career, after working in the telecommunications field, and I love getting students excited about science. I’ve even earned a few awards for being successful at it. I’m married to the love of my life, Jill, who is also a teacher. In our lives are three grown children and seven grandchildren. With great blessings, I share that they are all healthy, happy, and live close enough for us to see them regularly. At home we have replaced the kids with two cats and a dog.

My wife Jill with grandson Rion
My wife Jill with grandson Rion
Jills husband - me, John Clark
Jills husband – me, John Clark
Sabi dog in the pool with granddaughter Morgan
Sabi dog in the pool with granddaughter Morgan

In a few days, anticipation will be replaced by action as I board a plane headed for my NOAA Teacher at Sea experience I’ve waited for all summer to begin. I’ll be sailing aboard NOAA Ship Henry B. Bigelow, a ship specially built for NOAA to carry out the type of fisheries research I’ll be taking part in. I’ll be working side by side with experienced scientists who not only are knowledgeable in how to do the research conducted on board but also have the skill to share their knowledge with volunteers like me who have limited background in the science behind the work. It is the experience of a lifetime that I hope will energize my students about studying science as we carry out lesson plans developed from the experience and I share with them the stories of my time at sea. I’m sure a giant boat-eating squid will be in there somewhere.

NOAA Ship Henry B. Bigelow
NOAA Ship Henry B. Bigelow

Officially, I’m taking part in 2013 Autumn Bottom Trawl Survey conducted by the Ecosystems Survey Branch of the NOAA Fisheries Service. That’s a long fancy way of saying that the ship is going to drag a net for a short period of time near the bottom of the ocean and then collect data on the types of fish we catch as well as the environment they live in. Affectionately called a “critter cruise”, I now join a long line of Teacher at Sea alumni who have taken part in the biannual surveys of North Atlantic marine life. And there are a lot of critters to learn to identify as I’m finding out from watching the CD I was sent to be better prepared to support the research team. There are two types of Dogfish which look suspiciously like little sharks, flounders that are left eyed or right eyed depending on which side they decided to leave up, and squid distinguished by the length of a pair of fins down the side of the body. All you do is hold them upright, tentacles hanging toward the ground, and take a look. And don’t forget the large lump fish which is described as have the texture of a dog’s chew toy. Whatever the species, the role of the research volunteer is to sort them out and then collect data for the scientists to study.

Scientist sorting a catch aboard the FSF Henry B. Bigelow
Scientists sorting a catch aboard the Bigelow

What can be overlooked in the preparation is the part about how to handle fish. I do not like to touch fish so I will be facing my fears even while wearing gloves. And I really don’t like it when they flop around. I envision I’ll be the one with the hand in the wrong place when the shark twists around to see who is holding its tail or, at a minimum, squeeze too hard on the species that will poke you with a poison spine if you upset them. Other good advice I’ve learned from the CD is that there is a 100% recovery from seasickness and if the seas get rough, wedge yourself into your bunk with your life vest so you don’t roll around and fall out. My two year old granddaughter, Ireland, was watching the video with me while I studied and all she could say was “Oh my.”

Run, it's the dogfish!
Run, it’s the dogfish!

Britta Culbertson, Big Fish Little Fish, Sept 15, 2013

NOAA Teacher at Sea
Britta Culbertson
Aboard NOAA Ship Oscar Dyson
September 4-19, 2013

Mission: Juvenile Walleye Pollock and Forage Fish Survey
Geographical Area of Cruise: Gulf of Alaska
Date: Saturday, September 15th, 2013

Weather Data from the Bridge 
Wind Speed: 11kts
Air Temperature: 12.2 degrees C
Relative Humidity: 87%
Barometric Pressure: 1010.7 mb
Latitude: 59 degrees 26.51″ N              Longitude: 149 degrees 47.53″ W

Science and Technology Log

Finally, as we near the end of the cruise, I’m ready to write about one of the major parts of the survey we are doing.  Until now, I’ve been trying to take it all in and learn about the science behind our surveys and observe the variety of organisms that we have been catching. In my last few entries, I explained the bongo net tow that we do at each station.  Immediately after we finish pulling in the bongo nets and preparing the samples, the boat repositions on the station and we begin a tow using an anchovy net.  It gets its name from the size of fish it is intended to capture, but it is not limited to catching anchovies and as you will see in the entry below, we catch much more than fish.

 Why are we collecting juvenile pollock?

We are interested in measuring the abundance of juvenile pollock off of East Kodiak Island and in the Semidi Bank vicinity.  We are not only focusing on the walleye pollock, we are also interested in the community structure and biomass of organisms that live with the pollock.  Other species that we are measuring include: capelin, eulachon, Pacific cod, arrowtooth flounder, sablefish, and rockfish.  As I described in the bongo entries, we catch zooplankton because those are prey for the juvenile pollock.

Pollock trio
On the top is an age 2+ pollock, below that an age 1 pollock, and then below that is an age zero pollock. (Photo credit: John Eiler)

The Gulf of Alaska juvenile walleye pollock study used to be conducted every year, using the same survey grid.  Now the Gulf of Alaska survey is conducted every other year with the Bering Sea surveyed in alternating years.  That way, scientists can understand how abundant the fish are and where they are located within the grid or study area.  With the data being collected every year (or every other year), scientists can establish a time series and are able to track changes in the population from year to year. The number of age 0 pollock that survive the winter ( to become age 1) are a good indicator of how many fish will be available for commercial fisheries. NOAA’s National Marine Fisheries Service (NMFS) will provide this data to the fisheries industry so that fishermen can predict how many fish will be available in years to come.  The abundance of age one pollock is a good estimate of fish that will survive and be available to be caught by fishermen later, when they reach age 3 and beyond, and can be legally fished.

The other part of our study concerns how the community as a whole responds to changes in the ecosystem (from climate, fishing, etc.).  That is why we also measure and record the zooplankton, jellyfish, shrimp, squids, and other fish that we catch.

How does it work?

The anchovy net (this particular design is also called a Stauffer trawl) is pretty small compared to those that are used by commercial fishermen.  The mesh is 5 millimeters compared to the 500 micrometer mesh that we used for the bongo.  The smallest organisms we get in the anchovy net are typically krill.

Trawl net
A picture of a generic trawling net. It’s very similar to the anchovy net that we are using.

Typically, we don’t catch large fish in the net, but there have been some exceptions.  You might wonder why larger fish do not get caught in the net. It’s because the mesh is smaller and it’s towed through the water very slowly.  Fish have a lateral line system where they can feel a change in pressure in the water.  The bow wave from the boat creates a large pressure differential that the fish can detect.  Larger fish are usually fast enough to avoid the net as it moves through the water, but small fish can’t get out of the way in time.  One night we caught several Pacific Ocean Perch, which are larger fish, but very slow moving.  They are equipped with large spines on their fins and are better adapted to hunkering down and defending themselves as opposed to other fish that are fast swimmers and great at maneuvering.

Pacific Ocean Perch
This is one of the Pacific Ocean Perch (rockfish) that got caught in our net.

When we pull in the trawl net, it is emptied into buckets and then the haul is sorted by species and age class.  The catch is then measured, weighed, and recorded on a data sheet.  After that, we return most of the fish to the sea and save 25 of the juvenile pollock, capelin, and eulachon to take back to Seattle for further investigation.  We also save some of the smaller flatfish and sablefish to send back to Seattle. Check out the gallery below to see the process from beginning to end.

This slideshow requires JavaScript.

Where are the pollock in the food web?

Eulachon and capelin are zooplanktivores and compete with the juvenile pollock for food. Larger eulachon and capelin are not competitors (those over 150 mm).  Arrowtooth flounder and Pacific Cod are predators of the juvenile walleye pollock.  Cyanea and Chrysaora jellyfish are also zooplanktivores and could potentially compete with juvenile walleye pollock, so that is why we focus on these particular jellyfish in our study.

 What’s in that net?

When we pull in the trawl, we sort it into piles of different species and different age classes.  If we get a lot of juvenile pollock (age 0), we measure and weigh 100 and freeze 25 to take back to the lab so their stomach contents can be examined.  We do the same procedure for young capelin, eulachon, and flatfish.  Other organisms like jellyfish are counted and weighed and put back in the ocean.

Below is a list of different organisms we have found in the anchovy net during this cruise:

  • Walleye Pollock
  • Eulachon
  • Capelin
  • Shrimp
  • Larger zooplankton
  • Pink and Coho Salmon
  • Pacific Ocean Perch
  • Lanternfish
  • Prowfish
  • Arrowtooth Flounder
  • Cyanea Jellyfish
  • Chrysaora Jellyfish
  • Miscellaneous clear jellyfish (some moon jellyfish)
  • Ctenophores (comb jellyfish)
  • Spiny Lumpsucker
  • Toad Lumpsucker
  • Grenadier
  • Flathead sole
  • Pacific cod
  • Herring
  • Sablefish
  • Sand Fish
  • Octopus
  • Snail fish

Personal Log

As we wind down the cruise, I’m feeling a little sad that it’s ending.  I’m looking forward to going home and seeing my husband and our dog, but I’ll miss the friends I’ve made on the ship and I’ll certainly miss collecting data.  Even though it can be quite repetitive after awhile, I can’t think of a more beautiful place to do this work than the Gulf of Alaska.  The last few days we have had a couple of stations near the coastline around Seward, Alaska and we have ventured into both Harris Bay and Resurrection Bay.  There we caught sight of some amazing glaciers and small islands.  There was even an island that had bunkers from WWII on it.  Yesterday, 3 Dall’s Porpoises played in our bow wake as I stood on the bridge and watched.  It’s moments like this that all of the discomforts of being at sea fall away and I can reflect on what an incredible experience this has been!

Glacier
Beautiful scenery from Resurrection Bay.
Dall's Porpoise
Three Dall’s porpoises that were playing in our bow wake.

 

Did You Know?

Spiny lumpsuckers are tiny, cute, almost spherical fish that have a suction disk on their ventral (bottom) side.  The suction disk is actually a modified pelvic fin.  They use the suction disk to stick to kelp or rocks on the bottom of the ocean.

Their family name is Cyclopteridae (like the word Cyclops!).  It is Greek in origin.  “Kyklos” in Greek mean circle and “pteryx” means wing or fin.  This name is in reference to the circle-shaped pectoral fins that are possessed by fish in this family.

These lumpsuckers are well camouflaged from their predators and their suction disk helps them overcome their lack of an air bladder (this helps fish move up and down in the water).  Because lumpsuckers don’t have an air bladder, they are not great swimmers.

Spiny lumpsuckers are on average about 3 cm in length, but there are larger lumpsuckers that we have found, like the toad lumpsucker that you can see in the photo below.

You can read more about the spiny lumpsucker on the Aquarium of the Pacific’s website.

Louise Todd, Underway, September 16, 2013

NOAA Teacher at Sea
Louise Todd
Aboard NOAA Ship Oregon II
September 13 – 29, 2013

Mission: Shark and Red Snapper Bottom Longline Survey
Geographical Area of Cruise: Gulf of Mexico
Date: September 16, 2013

Weather Data from the Bridge:
Barometric Pressure: 1014.01mb
Sea Temperature: 28.8˚Celsius
Air Temperature: 29.9˚C
Wind speed: 19.22 knots

Science and Technology Log:

Oregon II
Oregon II (Photo Credit NOAA)

We left Galveston a little before 2pm on Sunday, September 15.  We were in transit to our first sampling location and should arrive there around 8pm tonight.  Depending on the conditions we might actually be able to do some fishing tonight!

Today we went through our abandon ship drill.  The ship’s alarm is used to alert everyone on board in the event of an emergency.  Abandon ship is indicated by 7 short rings followed by one long ring of the alarm.  When the alarm sounds with the abandon ship signal, we must carry our survival suits, personal flotation devices (PFDs), long pants, a hat and a long-sleeved shirt to the well deck, at the bow (front) of the ship.  My survival suit and personal flotation device (PFD) are kept in cabinets in my room.  The survival suit is tricky to get on and it gets very, very warm when you are wearing it!

Survival Suit
In my survival suit (Photo Credit Lisa Jones)

Personal Log:

During this initial transit, there hasn’t been much for me to do.  I spent a lot of time sleeping on Sunday.  The way the waves rock the ship back and forth makes me very sleepy!  I have taken a few short naps today in order to be ready in case we do any fishing on the later part of my shift tonight.  I am on the day shift which means I will work noon to midnight.  I think it will take me some time to get used to staying up that late but I think these naps will help!  As we start fishing the days will be much busier for me so staying awake will be easy I hope.  The views off of the ship are amazing.  I was surprised to see how blue the water gets.

View off the ship
View off the Oregon II

My stateroom is very comfortable and I have plenty of space in drawers and cabinets for everything I brought with me.  I am getting used to latching doors and drawers behind me so they do not slam back and forth as the ship rocks.  On the ship there is always someone sleeping so everyone works hard to be courteous and stay quiet.

My stateroom
My stateroom

My roommate is an officer on the ship so we are usually in the room at different times.  Officers on NOAA ships are part of the NOAA Corps.  Roommates are usually assigned based on the shifts people are working so each person has some time alone in the room.  As we start fishing more I will bring my computer and other items I might want throughout the day into one of the labs on the ship so I won’t have to go in and out of the room when my roommate might be sleeping.  The curtains are helpful in blocking out any light that might prevent you from sleeping.  The showers are right next to my room which is convenient and the common head (bathroom) is just around the corner.

There are plenty of food choices in the galley on the ship and everything has been delicious.  In the mornings you can even get eggs made to order!  I certainly don’t think I will be going hungry!

Did You Know?

Even in the warmer waters of the Gulf of Mexico, hypothermia is risk due to the difference in water temperature and our body temperatures.  The survival suit helps to protect our bodies from the difference in temperature.

 

Susy Ellison, A Hydrographic Wonderland, September 13, 2013

NOAA Teacher at Sea
Susy Ellison
Aboard NOAA Ship Rainier
September 9-26, 2013

Mission:  Hydrographic Survey
Geographic Area: South Alaska Peninsula and Shumagin Islands
Date:  September 13, 2013

Weather:  current conditions from the bridge
You can also go to NOAA’s Shiptracker (http://shiptracker.noaa.gov/) to see where we are and what weather conditions we are experiencing
GPS Reading:  55o 15.037’ N  162o 38.025’ W
Temp: 10.44C
Wind Speed: 9.8 kts
Barometer: 1021.21 mb
Visibility:  foggy on shore

Science and Technology Log

Since leaving Kodiak 5 days ago, I have been immersed in a hydrographic wonderland.  Here’s what I’ve learned, summed up in two words (three, if you count the contraction); it’s complicated.  Think about it.  If I asked you to make a map of the surface of your desk you could, with a little bit of work and a meter stick, make a reasonably accurate representational diagram or map of that surface that would include the flat surface, as well as outlines of each item on the surface and their heights relative to that surface, as well as their location relative to each other on a horizontal plane.  You might want to get fancy and add notes about the type of surface (is it wood, metal, or some sort of plastic), any small irregularities in that surface (are there some holes or deep scratches—how big and how deep?), and information about the types of objects on the desk top (are they soft and squishy, do they change location?).  Now, visualize making this same map if your desktop was underwater and you were unable to actually see it.   Not only that, the depth of the water over your desktop can change 2 times each day.  If that isn’t complicated enough, visualize that the top of the water column over your desk is in constant motion.  OK, not only all those variables, but pretend you are transformed into a very teeny person in a small, floating object on that uncertain water over the top of your desk trying to figure out how to ‘see’ that desktop that you can’t actually see with your own eyes?  Welcome to the world of the hydrographer; the challenge of mapping the seafloor without actually touching it.  It is, indeed, a complex meld of science, technology, engineering, and math (STEM, in educational parlance), as well as a bit of magic (in my mind).

How do you know what's down there?
How do you know what’s down there?

Challenge number one—how do you measure something you can’t see or touch with your own hands?  Long ago, sailors solved that obstacle by using a lead line; literally, a line with a lead weight attached to the end.  They would drop the weighted line over the side of their ship to measure the depth.  These soundings would be repeated to get enough data to provide a view of the bottom.  This information was added to their maps along with estimates of the horizontal aspects (shoreline features and distance from the shoreline) to create reasonably good charts that kept them off most of the underwater obstacles. A simple solution to a complex problem.  No electricity required, no advanced degrees in computer science needed, no calculus-based physics necessary.  Fast- forward to 2013 and the world of complex calculations made possible by a variety of computer-based algorithmic calculations (i.e. some darn fancy computing power that does the math for you). The NOAA Ship Rainier’s hydrographers use sound as their lead line, traveling in small boats known as launches that are equipped with multibeam sonar that send a series of sound ‘pings’ to the ocean floor and measures the time between sending and receiving the ping back after its trip to the bottom.  Sounds simple enough, doesn’t it?  If it were all that simple I wouldn’t be typing this in a room on the Rainier filled with 20 computer monitors, 10 hard drives, and all sorts of other humming and whirring electronic devices.  Not only that, each launch is equipped with its own impressive array of computer hardware.

One of the launches is lowered from the ship.
One of the launches is lowered from the ship.

So far on our survey days 2 launches have been sent out to cover identified transects.  Their onboard crew includes a coxswain (boat driver), as well as 2-3 survey technicians and assistants. Each launch is assigned a polygon to survey for the day.

EVERY PING YOU TAKE…

Once they arrive at their assigned area, it’s time to ‘mow the lawn’—traverse back and forth systematically collecting data from one edge of your assigned polygon to the other until the entire area has been surveyed. Just in case you haven’t realized it yet, although that sounds pretty straightforward, it isn’t. Is the area shallow or deep?  Depth affects how much area each traverse can cover; the sonar spreads out as it goes downward sending it’s little pings scampering to the ocean floor. Visualize an inverted ‘V’ of pings racing away from the sonar towards the sea floor. If it’s deep, the pings travel further before being bounced back upwards.  This means that the width of each row the sonar cuts as it “mows the lawn” is wider in deeper water, and narrower in shallow.  Shallower areas require more passes with the launch, since each pass covers a more limited area than it might if the water were deeper.  As the launch motors back and forth ‘mowing the lawn’, the sonar  signature is recorded and displayed on monitors in the cabin area and in front of the driver.  Ideally, each lap overlaps the previous one by 25-50%, so that good coverage is ensured.  This requires a steady hand and expert driving skills as you motor along either over or parallel to ocean swells.  All you video gamers out there, take note–add boat driving to the repertoire of skills you might need if you want to find a job that incorporates video gaming with science!

sonar screen
One of the monitors displays the sonar. The green line is the seafloor. This image shows that the deeper the sea, the wider the swath that is covered with each pass of the launch.
Calvin Burch uses a computer monitor to guide him as he drives the launch.  It's an art to 'mow' in straight lines while anticipating every roll and bounce of the coean's surface.
Calvin Burch uses a computer monitor to guide him as he drives the launch. It’s an art to ‘mow’ in straight lines while anticipating every roll and bounce of the ocean’s surface.

Here’s a small list of some of the variables that need to be considered when using sonar to calculate depth; the chemistry of the water column through which you are measuring, the variability of the water column’s depth at specific times of day, the general depth (is it shallow or deep), and the movement of the measuring device itself.  So many variables!!

Starla Robinson and Randy Shingeldecker monitor our progress on the launch's computer monitors.
Starla Robinson and Randy Shingledecker set up the program that will enable them to monitor our progress

HOW FAST DOES SOUND TRAVEL?

When you’re basing your charts on how sound travels through the water column, you need to look at the specific characteristics of that water.  In a ‘perfect world’, sound travels at 1500m/second through water.  In our real world, that speed is affected by salinity (the concentration of salts), temperature, and depth (water pressure).  The survey crew uses a CTD meter to measure Conductivity, Temperature, and Depth.  The CTD meter is deployed multiple times during the day to obtain data on these parameters.  It is attached to a line on the rear of the launch, dropped into the water just below the surface for 2 minutes, and then lowered to near the ocean floor to collect data.  After retrieval, it’s hooked to the computer on the launch to download the data that was collected.  That data is stored in its own file to use when the data is reviewed in the evening back on board the Rainier.  This is one of the variables that will be applied to the sonar data file—how fast was the sound moving through the water?  Without this information to provide a baseline the sonar data would not be accurate.

ctd deploy 1
Randy Shingledecker gets ready to send the CTD over the side. It’s clipped into a stout line and a reel for lowering it.
ctd retrieval 1
The CTD is lowered to just above the seafloor to collect data on Conductivity, Temperature, and Depth. This data will be applied to our sonar data to obtain an accurate sound speed for this area.


 

 

 

ROCKING AND ROLLING…

When you’re out on the ocean in a boat, the most obvious variable is the instability of the surface, itself.  This is called ‘attitude’.  Attitude includes changes to the boat’s orientation fore and aft (pitch), side-to-side (roll), and up and down (heave) as it is gently, and not-so-gently rocked by ocean swells and waves.  This means that the sonar is not always where you think it is in relation to the seafloor.  This is like trying to accurately measure the height of something while you, the measurer, are on a surface that is constantly moving in 3 different directions. Good luck.  Luckily for this crew of hydrographers, each boat is equipped with a little yellow box whose technical name is the IMU (inertial measurement unit) that I call the heave-o-meter, as we bob up and down on this might ocean.  This little box contains 3 gyroscopic sensors that record all those forward and backward pitches, sideways rolls, as well as the bobbing up and down motions that the boat does while the sonar is pinging away.  This information is recorded in the launch’s computer system and is applied to the sonar data during analysis back at the Rainier.

This yellow box is the IMU.  It's internal gyros capture information about the boat's pitch, roll, and heave.
This yellow box is the IMU. It’s internal gyros capture information about the boat’s pitch, roll, and heave.

TIME AND TIDE…

Now that you’ve gotten your launch to the correct polygon (using GPS data to pinpoint your location), taken CTD readings to create a sound transmission profile for your transect area, and started up the heave-o-meter to account for rocking and rolling on the high seas, it’s time to start collecting data.  Wait—there’s still another variable to think about, one that changes twice daily and affects the height of the water column.  You also have to factor in changes in the depth of the water due to tidal changes. (for an in-depth look at how tides work, check out this link: http://oceanservice.noaa.gov/education/kits/tides/tides01_intro.html).  At high tide, there’s a greater likelihood that subsurface obstacles will be covered sufficiently.  At low tide, however, it’s pretty important to know where the shallow spots and rocks might lurk.  NOAA’s hydrographers are charting ocean depths referenced to mean lower low water, so that mariners can avoid those low-water dangers.

You might be asking yourself, who keeps track of all that tide data and, not only that, how do we know what the tide highs and lows will be in an area where there are no other tide gauges?   NOAA has tide gauges along many coastal areas.  You can go online to http://tidesandcurrents.noaa.gov/and find out predicted tide heights and times for any of these locations.  While we are working here in Cold Bay, we are using a tide gauge in nearby King Cove, as well as a tide gauge that the Rainier’s crew installed earlier this summer.  More data is better.

Here's the tide chart from the King Cove tide gauge.
Here’s the tide chart from the King Cove tide gauge.

What do you do if you’re surveying in an area that doesn’t have existing tide gauges?  In that case, you have to make your own gauge that is referenced to a non-moving point of known elevation (like a rock).  For a detailed description of how these gauges are set, check out NOAA TAS blogs from some of the teachers who preceded me on the Rainier. On Wednesday, I helped dismantle a tide gauge on Bird Island in the Shumagin Islands that had been set up earlier this season (check out TAS Avery Martin’s July 12th posting), but had ceased to report reliable data.  Our mission on Wednesday was to find out if the station had merely stopped reporting data or if it had stopped collecting data entirely. 

Setting off in a skiff to check on the Bird Island tide gauge.
Setting off in a skiff to check on the Bird Island tide gauge.

When we arrived at Bird Island we found out exactly why the gauge had stopped sending data—its battery bank had fallen from one rocky ledge to another, ripping apart the connections and breaking one of the plastic battery boxes in the process.  That took a lot of force—perhaps a wave or some crazy gust of wind tore the 3 batteries from their mooring.  Since each battery weighs over 25lbs, that means that something moved over 75lbs of batteries.  Ideally, the station uses solar panels to keep the batteries charged.  The batteries power up the station so that data can be sent to a satellite. Data is also stored on site in a data logger, but without power that data logger won’t work.

This is the data logger for the tide gauge.  It is housed in a watertight box and was retrieved for downloading on the ship.
This is the data logger for the tide gauge. It is housed in a watertight box and was retrieved for downloading on the ship.

We retrieved all the equipment and will be able to download whatever data had been recorded before the system broke. The automated tide gauge is, basically, a narrow diameter air-filled tube that is underwater and set at a fixed depth with a narrow opening pointed downward to the seafloor. The pressure required to balance the air in the tube is equal to the pressure of the water column directly above the opening.  The tide gauge measures this pressure and converts it to depth.  Pressure/depth changes are recorded every six minutes—or ten times each hour. As it turns out, the damaged battery bank was only one of the problems with this station.  Problem number two was discovered by the dive team that retrieved the underwater portion of the gauge; the hose had been severed in two locations. In this case, something had caused the tube to break, so it was no longer connected to the data logger.  That must have been some storm!

ENC Carrier inspects the battery bank that inow s on a rock ledge 2 feet below where it had been placed!
ENS Carrier inspects the battery bank that rests on a rock ledge 2 feet below where it had been placed weeks ago!
The waterproof battery boxes were broken in the tumble.
The waterproof battery boxes were broken in the tumble.
The solar panels that charged the batteries were intact, still tied into bolts in the rocks.
The solar panels that charged the batteries were intact, still tied into bolts in the rocks.
The dive crew gets ready to jump in
The dive crew gets ready to jump in
Brrr, it's chilly work diving in arctic waters.  The divers are investigating the gauge and removing the damaged hose
Brrr, it’s chilly work diving in arctic waters. The divers are investigating the gauge and removing the damaged hose

While there, we set to work checking on benchmarks that had been set earlier in the season.  We used a transit and survey rods (oversized rulers) to measure the relative heights of a series of benchmarks to ensure accuracy. There are 5 benchmarks along the beach.  Each one was surveyed as a reference to the primary benchmark nearest the gauging station.  Multiple measurements help ensure greater accuracy.

I am holding the survey rod on top of a benchmark.
I am holding the survey rod on top of a benchmark.

 

I used a level to make sure the rod was plumb--perpendicular to the benchmark.  No easy feat with a strong wind blowing!
I used a level to make sure the rod was plumb–perpendicular to the benchmark. No easy feat with a strong wind blowing!

We also were tasked with checking the primary benchmark’s horizontal location.  While this had been carefully measured when it was set back in July, it’s important to make sure that it hasn’t moved.  It might seem a crazy concept to think that a benchmark cemented into a seemingly immovable piece of rock could move, but we are in a region that experiences seismic events on an almost daily basis.  (You can check out seismic activity at http://www.aeic.alaska.edu/) NOAA Corps Officer ENS Bill Carrier set up a GPS station at the benchmark to collect 4 hour’s data on its position, a process called HORCON (horizontal control).  Unfortunately, the winds were in charge of how much data we were able to collect that day, and blew down the station after only 3 hours! [image of station down]  Sometimes the best laid plans …..

A gust of wind blew the recording station down.
A gust of wind blew the recording station down.

 

DATA, DATA, and MORE DATA

While data collection is important, it’s what you do with the data that really gets complicated.  Data management is essential when working with so many files and so many variables. Before each launch returns to the Rainier, the day’s data is saved onto a portable hard drive.  Immediately after being hauled back up onto the ship, the data is handed off to the ‘Night Processing Team’ and hustled off to the Plotting Room (computer HQ) to be uploaded into a computer.  This is where the magic happens and an advanced degree in computer science or GIS (geographic information systems) can come in handy.  I have neither of those qualifications, but I know how to read a screen, click a mouse, and follow directions.  So, on Friday evening I was ushered into the ranks of ‘night processor’.

When each launch returns to the ship, their day's data is saved onto a hard drive.  This drive is transported to the plotting room to download onto the computer.
When each launch returns to the ship, their day’s data is saved onto a hard drive. This drive is transported to the plotting room to download onto the computer.

First, data is downloaded into the main computer.  Each launch’s files are called raw data files and are recorded in the launch’s acquisition logs.  Once the data is on the computer, it is important to set up what I call a ‘file tree’; the series of files that increase in specificity.  This is analogous to having an accurate list of what files live within each drawer and section of your file cabinet. These files are color-coded according to the operations manual protocols to minimize the chance of misfiling or the data.  They are definitely more organized than the files on my laptop—I might change my lackadaisical filing ways after this trip!

Once the data are placed in their folders, the fun begins.  Remember, you have files for multiple variables;  sonar, CTD casts, the IMU Heave-o-meter, and tide data.  Not only that, you have, with any luck, performed multiple casts of your CTD meter to obtain accurate data about the conditions affecting sound wave transmission within your polygon.  Now you get to do something I have never done before (and use a vocabulary word I never knew existed and one that I might try to spell in a future Scrabble game); you concatenate your CTD data.  Basically, you put the data from all your CTD casts together into one, neat little file.  Luckily, the computer program that is used does this for you.  Next, you direct the program to add all the variables to your sonar files; the concatenated CTD data, tide data, and IMU data.

 

Survey Tech Brandy Geiger and ENS Wall begin to upload the data and organize it into files.
Survey Tech Brandy Geiger and NOAA Corpsman ENS Wall begin to upload the data and organize it into files.

Assuming all goes well and you have merged all your files, it’s time to ‘clean’ your data and review it to make sure there are no obvious holes or holidays in the data that was collected.  Holidays can occur if the launch was bouncing too much from side to side during data collection and show up as a blank spot in the data because the sonar was out of the water and not pinging off the bottom.  You can identify these holidays during the data collection process [holiday signature], but sometimes there are smaller holidays that show up once the data is merged and on your computer screen.  There can also be miscellaneous errant pings caused by debris in the water column.  Cleaning involves systematically searching each line of your surveyed polygon to identify and delete those ‘bad’ pings.  Kind of like photoshopping away the parts of a digital image that you don’t want in the final image.  You work methodically in a grid pattern from left to right and top to bottom to ensure that you are covering the whole file.  It sounds easy, but to a non-PC person such as myself all that right click, left click, center click stuff was a bit boggling.  The program is amazingly complex and, rumor has it, a little bit ‘buggy’ at times.

Multiple screens, multiple tasks.  I am learning the art of 'cleaning' the data--getting rid of extraneous pings.
Multiple screens, multiple tasks. I am learning the art of ‘cleaning’ the data–getting rid of extraneous pings.


After all this, guess what?!  You still don’t have a chart.  It takes almost 2 years to go from data collection to chart publication.  There’s endless amounts of data compilation, reports to be written, and quality control analysis to be completed before the final report and charts are issued.

Personal Log

So far I have spent two nights on the ship ‘in transit’, moving between ports. The other nights have been spent anchored offshore. While the first night at sea was a little bouncy, the second was, in my opinion, the wildest roller coaster ride I have ever taken.  Imagine being pulled to the top of a high roller coaster, and released to fly down to the bottom while you are lying flat in your bed.  That’s what it felt like as we motored from the Shumagin Islands to an anchorage in Cold Bay.  An endless series of up, up, ups, followed by a wild ride down, down, down. Luckily all the drawers and doors have latches that keep them from flying open—although I had a jacket hanging on a hook that seemed to hit the latch on one closet door and actually knock it open—after this happened a couple of times I gave up and put the coat on the floor and firmly shut the door.  My bathroom trash can ended up in the shower stall.  At one point I heard a loud thump in the dark—and realized my survival suit in its orange bag had fallen from the top bunk to the floor—glad I wasn’t in its way! It was time to just hang on and try not to roll out of bed.

If your chair isn't tied down, put tennis balls over the wheels to keep it from rolling!
If your chair isn’t tied down, put tennis balls over the wheels to keep it from rolling!
tiedown1
Strap the printer tightly to a table!
tiedown2
Don’t forget to secure the trashcans!

We finally stopped rocking and rolling around 3 in the morning.  I thought maybe I was just a bit sensitive to the rocking motion, but was comforted to find out the everyone agreed that it had been a wild night.  In fact, one of the potential ‘hazards’ for our work on Thursday was ‘lack of sleep’.

FOO Meghan Mcgovern goes over the Plan of the Day (POD).  Today's identified hazards included 'Lack of Sleep'.
FOO LT Meghan McGovern goes over the Plan of the Day (POD). Today’s identified hazards included ‘Lack of Sleep’.

 

After almost a week aboard the Rainier I have been impressed with the teamwork, precision, and overall efficiency which overlays all operations. This crew can get a launch loaded, lowered, and underway in less time than it sometimes takes me to record my morning attendance at school!  This is no simple feat (the boat, not the attendance!).  It reminds me of a buzzing beehive filled with activity and focused on a single task; data collection. Each day begins on the fantail (the rear of the boat) at 0800 with the FOO (Field Operations Officer) reviewing the POD (Plan of the Day) and a summary of the day’s goals, work assignments, weather, and potential hazards, prior to sending out the survey crews.

The Boatswain (bo’sun) directs the next part of this tightly choreographed activity, as the launches are lowered by their davits (small cranes), while lines and hooks are handled with an eye to safety and efficiency.  Within 5 minutes the two launches have been lowered, loaded with crew and supplies, and are on the water, buzzing away from the hive like bees to perform their daily waggle dance as they move back and forth collecting hydrographic data.

At 1630 they return to the hive, filled with the sweet nectar of hydrographic data.  Launches are lifted back onto the ship and the data is whisked off to the computer room for downloading. 5 Minutes later a survey team debrief is held to review work accomplished that day and any problems that may have come up so that plans can be made for the next day’s work.  This crew is organized!!

The NOAA Ship Rainier
The NOAA Ship Rainier

 

 

 

Britta Culbertson: The Beat of the Bongo (Part 2) – Catching Zooplankton, September 12, 2013

NOAA Teacher at Sea
Britta Culbertson
Aboard NOAA Ship Oscar Dyson
September 4-19, 2013

Mission: Juvenile Walley Pollock and Forage Fish Survey
Geographical Area of Cruise: Gulf of Alaska
Date: Wednesday, September 12th, 2013

Weather Data from the Bridge (for Sept 12th, 2013 at 9:57 PM UTC):
Wind Speed: 23.05 kts
Air Temperature: 11.10 degrees C
Relative Humidity: 93%
Barometric Pressure: 1012.30 mb
Latitude: 58.73 N              Longitude: 151.13 W

Science and Technology Log

Humpback Whale
A humpback whale. (Photo credit: NOAA)

We have been seeing a lot of humpback whales lately on the cruise.  Humpback whales can weigh anywhere from 25-40 tons, are up to 60 feet in length, and consume tiny crustaceans, plankton, and small fish.  They can consume up to 3,000 pounds of these tiny creatures per day (Source: NOAA Fisheries).  Humpback whales are filter feeders and they filter these small organisms through baleen.  Baleen is made out of hard, flexible material and is rooted in the whale’s upper jaw.  The baleen is like a comb and allows the whale to filter plankton and small fish out of the water.

Baleen
This whale baleen is used for filter feeding. It’s like a small comb and helps to filter zooplankton out of the water. (Photo credit: NOAA)

I’ve always wondered how whales can eat that much plankton! Three thousand pounds is a lot of plankton.  I guess I felt that way because I had never seen plankton in real-life and I didn’t have a concept of how abundant plankton is in the ocean. Now that I’m exposed to zooplankton every day, I’m beginning to get a sense of the diversity and abundance of zooplantkon.

In my last blog entry I explained how we use the bongo nets to capture zooplankton.  In this entry, I’ll describe some of the species that we find when clean out the codends of the net.  As you will see, there are a wide variety of zooplankton and though the actual abundance of zooplankton will not be measured until later, it is interesting to see how much we capture with nets that have 20 cm and 60 cm mouths and are towed for only 5-10 minutes at each location.  Whales have much larger mouths and feed for much longer than 10 minutes a day!

Cleaning the codends is fairly simple; we spray them down with a saltwater hose in the wet lab and dump the contents through a sieve with the same mesh size as the bongo net where the codend was attached.  The only time that this proves challenging is if there is a lot of algae, which clogs up the mesh and makes it hard to rinse the sample.  Also, the crab larvae that we find tend to hook their little legs into the sieve and resist being washed out.  Below are two images of 500 micrometer sieves with zooplankton in them.

Zooplankton
A mix of zooplankton that we emptied out of the codend from the bongo.
Crab larvae
Crab larvae (megalopae) that we emptied out of the codend.

Some of the species of zooplankton we are finding include different types of:

  • Megalopae (crab larvae)
  • Amphipods
  • Euphausiid (krill)
  • Chaetognaths
  • Pteropods (shelled: Limasina and shell-less: Clione)
  • Copepods (Calanus spp., Neocalanus spp., and Metridea spp.)
  • Larval fish
  • Jellyfish
  • Ctenophores

The other day we had a sieve full of ctenophores, which are sometimes known as comb jellies because they possess rows of cilia down their sides.  The cilia are used to propel the ctenophores through the water.  Some ctenophores are bioluminescent.  Ctenophores are voracious predators, but lack stinging cells like jellyfish and corals. Instead they possess sticky cells that they use to trap predators (Source:  UC Berkeley).  Below is a picture of our 500 micrometer sieve full of ctenophores and below that is a close-up photo of a ctenophore.

Ctenophores
A sieve full of ctenophores or comb jellies.
Ctenophore
A type of ctenophore found in arctic waters. (Photo credit: Kevin Raskoff, MBARI, NOAA/OER)

It’s fun to compare what we find in the bongo nets to the type of organisms we find in the trawl at the same station.  We were curious about what some of the fish we were eating, so we dissected two of the Silver Salmon that we had found and in one of them, the stomach contents were entirely crab larvae! In another salmon that we dissected from a later haul, the stomach contents included a whole capelin fish.

Juvenile pollock are indiscriminate zooplanktivores.  That means that they will eat anything, but they prefer copepods and euphausiids, which have a high lipid (fat) content. Once the pollock get to be about 100 mm or greater in size, they switch from being zooplanktivores to being piscivorous. Piscivorous means “fish eater.”  I was surprised to hear that pollock sometimes eat each other.  Older pollock still eat zooplankton, but they are cannibalistic as well. Age one pollock will eat age zero pollock (those that haven’t had a first birthday yet), but the bigger threat to age zero pollock is the 2 year old and older cohorts of pollock.  Age zeros will eat small pollock larvae if they can find them.  Age zero pollock are also food for adult Pacific Cod and adult Arrowtooth Flounder.  Older pollock, Pacific Cod, and Arrowtooth Flounder are the most voracious predators of age 0 pollock.  Recently, in the Gulf of Alaska, Arrowtooth Flounder have increased in biomass (amount of biological material) and this has put a lot of pressure on the pollock population. Scientists are not yet sure why the biomass of Arrowtooth Flounder is increasing. (Source: Janet Duffy-Anderson – Chief Scientist aboard the Dyson and Alaska Fisheries Science Center).

The magnified images below, which I found online, are the same or similar to some of the species of zooplankton we have been catching in our bongo nets.  Click on the images for more details.

Personal Log (morning of September 14, 2013)

I’m thankful that last night we had calm seas and I was able to get a full eight hours of sleep without feeling like I was going to be thrown from my bed.  This morning we are headed toward the Kenai Peninsula, so I’m excited that we might get to see some amazing views of the Alaskan landscape.  The weather looks like it will improve and the winds have died down to about 14 knots this morning.  Last night’s shift caught an octopus in their trawl net; so hopefully, we will find something more interesting than just kelp and jellyfish in our trawls today.

Did You Know?

I mentioned that we had found some different types of pteropods in our bongo nets.  Pteropods are a main food source for North Pacific juvenile salmon and are eaten by many marine organisms from krill to whales.  There are two main varieties of pteropods; there are those with shells and those without.  Pteropods are sometimes called sea butterflies.

Pteropod
A close-up of Limacina helicina, a shelled pteropod or sea butterfly. (Photo credit: Russ Hopcroft/University of Alaska, Fairbanks)

Unfortunately, shelled pteropods are very susceptible to ocean acidification.  Scientists conducted an experiment in which they placed shelled pteropods in seawater with pH and carbonate levels that are projected for the year 2100.  In the image below, you can see that the shell dissolved slowly after 45 days.  If pteropods are at the bottom of the food chain, think of the implications of the loss of pteropods for the organisms that eat them!

Pteropods
Shelled pteropods after being exposed to sea water that has the anticipated carbonate and pH levels for the year 2100. Notice the degradation of the shell after 45 days. (Photo credit: David Liittschwager/National Geographic Stock)

Read more about ocean acidification on the NOAA’s Pacific Marine Environmental Laboratory (PMEL) website. Also, check out this press release from November 2012 by the British Antarctic Survey about the first evidence of ocean acidification affecting marine life in the Southern Ocean.

Teacher’s Corner

In my last blog entry on the bongo, I talked about using the “frying pan” or clinometer to measure wire angle.  If you’re interested in other applications of clinometers, there are instructions for making homemade clinometers here and there’s also a lesson plan from National Ocean Services Education about geographic positioning and the use of clinometers this website.

If you are interested in teaching your students about different types of plankton, here is a Plankton Wars lesson plan from NOAA and the Southeast Phytoplankton Monitoring Network, which helps students to understand how plankton stay afloat and how surface area plays a role in plankton survival.

If you would like to show your students time series visualizations of phytoplankton and zooplankton, go to NOAA’s COPEPODite website.

Zooplankton time series
Zooplankton time series visualization from the COPEPODite website.

For more plankton visualizations and data, check out NOAA’s National Marine Fisheries Service website.

If you are interested in having your students learn more about ocean acidification, there is a great ocean acidification module developed for the NOAA Ocean Data Education Project on the Data in the Classroom website.

Britta Culbertson: The Beat of the Bongo (Part 1): Catching Zooplankton, September 11, 2013

NOAA Teacher at Sea
Britta Culbertson
Aboard NOAA Ship Oscar Dyson
September 4-19, 2013

Mission: Juvenile Walley Pollock and Forage Fish Survey
Geographical Area of Cruise: Gulf of Alaska
Date: Wednesday, September 11th, 2013

Weather Data from the Bridge (for Sept 11th, 2013 at 10:57 PM UTC):
Wind Speed: 4.54 kts
Air Temperature: 10.50 degrees C
Relative Humidity: 83%
Barometric Pressure: 1009.60 mb
Latitude: 58.01 N              Longitude: 151.18 W

Science and Technology Log

What is a bongo net and why do we use it?

As I mentioned in a previous entry, one of the aspects of this cruise is a zooplankton survey, which happens at the same stations where we trawl for juvenile pollock.  The zooplankton are prey for the juvenile pollock.  There are many types of zooplankton including those that just float in the water, those that can swim a little bit on their own, and those that are actually the larval or young stage of much larger organisms like crab and shrimp.  We are interested in collecting the zooplankton at each station because because we are interested in several aspects of juvenile pollock ecology, including feeding ecology.  In order to catch zooplankton, we use a device called a bongo net.  The net gets its name because the frame resembles bongo drums.

20bon
Diagram of a 20 cm bongo net set-up. (Photo credit: NOAA – Alaska Fisheries Science Center)

The bongo net design we are using includes 2 small nets on a 20 cm frames with 153 micrometer nets attached to them and 2 large nets on 60 cm frames with 500 micrometer nets.  The 500 micrometer nets catch larger zooplankton and the 153 micrometer nets catch smaller zooplankton.  In the picture above, there are just two nets, but our device has 4 total nets.  At the top of the bongo net setup is a device called the Fastcat, which records information from the tow including the depth that bongo reaches and the salinity, conductivity, and temperature of the water.

Bongo in water
This is what the bongo looks like when it’s finally in the water (Photo credit: John Eiler)

What happens during a bongo net tow?

The process of collecting zooplankton involves many people with a variety of roles.  It usually takes three scientists, one survey tech, and a winch operator who will lower the bongo net into the water.  In addition, the officers on the bridge need to control the speed and direction of the boat.  All crew members are in radio contact with each other to assure that the operation runs smoothly.  Two scientists and a survey tech stand on the “hero deck” and work on getting the nets overboard safely.  Another scientist works in a data room at a computer which monitors the depth and angle of the bongo as it is lowered into the water.  It is important to maintain a 45 degree angle on the wire that tows the bongo to make sure that water is flowing directly into the mouth opening of the net.  One of the scientists on the hero deck will use a device that we lovingly call the “frying pan,” but more accurately it is called a clinometer or inclinometer. The flat side of the device gets lined up with the wire and an arrow dangles down on the plate and marks the angle.  The scientist calls out the angle every few seconds so that the bridge knows whether or not to increase or decrease the speed of the ship in order to maintain the 45 degree angle necessary.

Peter and the pan
Scientist Peter Proctor holds up the “frying pan” also known as a clinometer or inclinometer, which is used to measure the wire angle of the bongo when it’s in the water.

Meanwhile, back at the computer, we monitor how close the bongo gets to the bottom of the ocean.  We already know how deep the ocean is at our location because of the ship’s sonar.  The bongo operation involves a bit of simple triangle geometry.  We know the depth and we know the angles, so we just have to calculate the hypotenuse of the triangle that will be created when the bongo is pulled through the water to figure out how much wire to let out.  The survey tech uses a chart that helps him determine this quickly so he knows what to tell the winch operator in terms of wire to let out.  In the images below, you can see what we are watching as the bongo completes its tow.  The black line indicates the depth of the bongo, and the red, purple, and blue lines indicate temperature, conductivity, and salinity.

Good bongo tow
This is an example of a good bongo tow. The black line on the left of the graph shows a consistent tow angle both up and down. The key is that the black line should have a “v” shape on the graph if the tow is good.
Bad bongo
This graph shows what happens when a bongo gets caught in the current and stays at the same depth for a while. Look at how the black line isn’t smooth, but levels off for a bit. This happened with the bongo both when it was going down and coming back up to the surface.

When the bongo is within in 10 meters of the bottom, the survey tech radios the winch operator to start bringing the bongo back up.  It usually takes longer for it to come up as it does for it to go out, nevertheless, the 45 degree wire angle needs to be maintained.  When the survey tech sees the bongo at the surface of the water, the two scientists on the hero deck get ready to grab it.  This operation can be quite difficult when it’s windy and the seas are rough. If you look at the sequence of the photos below, pay attention to the horizon line where the water meets the sky and you can get a sense of the size of the swells that day.

When the bongo is safely back on deck, the person in the data room records the time of the net deployment, how long it takes to go down and up, how much wire gets let out, and the total depth at the station.  If anything goes wrong, this is also noted in the data sheet.

As the bongo reaches the surface, the scientists grab the net keep it from banging into the side of the ship.  When the net is on board, the next step is to read the flowmeters on the nets that indicate how much water has flowed through them.  Then we rinse the nets and wash all of the material down the nets and into the “codends” at the very end of the net.  These are little containers that can be detached and emptied to collect the samples.

Once the codends are detached, they are taken to the wet lab and rinsed.  Each of the four parts of the net has a codend where the zooplankton are caught. The zooplankton are rinsed out of the codends into a sieve and then collected in a jar and preserved with formalin.  The purpose of having two of each of the 20 cm and 60 cm bongo nets is to ensure that if one sample is bad or accidentally dumped, there is always a backup.  I have had to use the backup once or twice when there was a big jellyfish in the codend that kept me from getting all of the zooplankton out of the sample.

Codend
The codend from the 150 micrometer bongo net.
cleaning the codends and sieve
Britta rinsing the 500 micrometer sieve.

After we collect the zooplankton the samples are shipped to Seattle when we return to port. Back in the labs, the samples are sorted, the zooplankton are identified to species, and the catch is expressed at number per unit area.  This gives a quantitative estimate of the density of plankton in the water.  A high density of the right types of food means a good feeding spot for the juvenile walleye pollock!  This sorting process can take approximately one year.  I think it’s pretty amazing how much work goes into collecting the small samples we get at each station.  Just to think of all of the person hours and ship hours involved makes me realize how costly it is to study the ocean.

Colleen and zooplankton jar
Scientist Colleen Harpold holding up one of the preserved jars of zooplankton.
Colleen with zooplankton
Scientist Colleen Harpold holding up one of the preserved jars of zooplankton that has A LOT of algae in it too!

Personal Log

It is hard to believe that I’ve been on the ship a week now.  It feels strange that just 7 days ago I had never heard of a bongo net or an anchovy net.  Now I see them every day and I know how to identify several types of fish, jellyfish, and zooplankton.  I love working with the scientists and learning about the surveys we are doing.  Nearly every trawl reveals a special, new organism, like the Spiny Lumpsucker – go look that one up, I dare you!  We don’t have much down time and I’m trying to blog in between stations, but sometimes the time between stations after we finish our work can be 45 minutes and sometimes just 15 minutes.  So we are pretty much on the go for the whole 12-hour shift.  That’s where the fortitude part of Teacher at Sea comes in.  You definitely need to have fortitude to endure the long hours, occasional seasickness (I like to think of it as “sea discomfort”), and periodic bad weather.

By now though, it all seems routine and I’d like to think I’ve gotten used to being thrown around in my sleep a little now and again when we hit some rough seas.  This experience has been so worthwhile and even though I look forward to the comforts of home, I don’t really want it to end.  When I graduated from college, I worked with a herpetologist studying lizards in the desert south of Carlsbad, New Mexico.  I have fond memories of living in a tent for four months and collecting lizards all day to bring back to camp to measure and check for parasites.  I often miss doing scientific work, so Teacher at Sea has given me the opportunity to be a scientist again and to learn about a whole new world in the ocean.  What a treat! One of the reasons I chose to be a teacher was to be able to share my excitement about science with students and I feel so lucky that I get to share this experience too.

Did you know?

There are two species of Metridia, a type of copepod (zooplankton), that are found in the Gulf of Alaska/Bering Sea.  One of them is called Metridia lucens and the other one is Metridia oketensis.  These copepods are bioluminescent, which means that they glow when they are disturbed.  They sometimes glow when they are in the wake of the ship or on the crest of a wave.  Tonight when I was draining a codend into a sieve, my sieve looked like it had blue sparkles in it, but just for a second!  I asked our resident zooplankton expert, Colleen Harpold what they might be and she thought that my blue sparkles likely belonged to the genus Metridia.

If you are interested in reading a little more about Metridia, check out this blog from Scientific American on copepods in the Bering Sea!

Metridia longa
This is an image of Metridia longa. (Photo credit: NOAA/Hopcroft)
Glowing Metridia
This is a picture from Scientific American of Metridia spp. glowing while in a sieve. (Photo Credit: Chris Linder, Woods Hole Oceanographic Institute)

 Thanks for reading! Please leave me some comments or ask questions about any of the blog posts and feel free to ask other questions about the work we are doing or what it’s like at sea! I would love to be able to answer real-time while I am at sea.

Susy Ellison: There’s a Volcano Outside My Window, September 10, 2013

NOAA Teacher at Sea
Susy Ellison
Aboard NOAA Ship Rainier
September 9-26, 2013

Mission:  Hydrographic Survey
Geographic Area: South Alaska Peninsula and Shumagin Islands
Date:  September 10, 2013

Weather:
Partly cloudy
GPS Coordinates   540 49.627’  N ,   159o 46.421’  W
Temp. 10.3C
Wind Speed 10-14 kts
Barometer 1008.49 mb

Science and Technology Log

You never know what you might see first thing in the morning! When I awoke and looked out my porthole I saw this in the distance.

The volcano has been active for the past few months, but I saw no smoke today.  You can check out volcanic activity at  http://www.avo.alaska.edu/activity/Veniaminof.php
The volcano has been active for the past few months, but I saw no smoke today. You can check out volcanic activity at http://www.avo.alaska.edu/activity/Veniaminof.php

 

We  are scheduled to leave Kodiak at 1000 Hrs, RST
We are scheduled to leave Kodiak at 1000 Hrs, RST


We cast off yesterday morning at 1000 hrs, RST—Rainier Ship Time.  Although we are still in the Alaska Daylight Savings time zone, our time on the ship has been adjusted backwards 1 hour to give us more daylight during ‘working hours’.  Since the ship is its own floating universe, time that is referenced to a specific time zone is not as important as time that is referenced to our day and the work that needs to be completed.  Einstein would be pleased to see that time is, indeed, relative here aboard the Rainier!

There is science involved just to leave port and set forth on this cruise.  There’s data to be collected, such as a weather forecast—and decisions to be made based on that data.  Today’s weather report called for rain and high winds.  That data input resulted in a travel plan including taking a more protected route north of Kodiak Island instead of heading out to more open water right away.  We didn’t reach the wide-open spaces until evening, and I was lulled to sleep by the endless rocking and rolling of the boat.

We need to take out the trash before we leave.
We needed to take out the trash before we left.
Heading into the Shelikof Strait
Heading into the Shelikof Strait

Science can also include the protocols needed to keep everyone on board safe and healthy during a cruise.  With that in mind, I spent part of the day learning about the ship and the safety routines we need to follow.  Ensign Wall gave me my survival suit, aka Gumby Suit and showed me how to don that lifesaving apparel.  The suit is a foam-filled drysuit, providing insulation and floatation in one handy, non-form-fitting package.  They are, apparently, one size fits none, but when it’s a matter of survival, I doubt that style counts for too many points!

Each person aboard is assigned stations to report to in case of fire or in case it becomes necessary to abandon ship.  I found out that I go to the Boat Shop near the stern in case of fire, and that I head to Station 1 near the bridge.  We had a fire drill in the afternoon, followed by an abandon ship drill.  Much like fire drills at school, it’s a good time to practice and figure out the best way to get to where you need to go.  Since I’m still learning my way around the ship, it was especially important to figure out where I needed to go and how to get there.

Where do I go?
Where do I go?
Trying on my Gumby suit
Trying on my Gumby suit

Then there’s the ‘real’ science—the science of hydrography and the point of this entire venture.  The NOAA Ship Rainier has been tasked with charting (creating maps) of the Shumagin Islands and Cold Bay areas. It’s amazing to think that there are still some parts of our coastline that haven’t been charted.  I spent much of this afternoon talking with the scientists who are making these maps and came away with the overwhelming sense that this is, indeed, a complicated and multi-faceted process. I’ll be writing separate journals on all the science that goes into creating these detailed maps of the ocean floor.  If you just can’t wait and need to know more right now, check out the blogs from previous TAS teachers on the Ship Rainier.

Personal Log

Much of my first day at sea was spent getting used to being aboard a large floating object on a rather bumpy sea.   Our day was spent in transit, from Kodiak to the Shumagin Islands, around 28 hours away.

My very first rainbow at sea!
My very first rainbow at sea!

There’s a lot to learn about life on board the Rainier.  Most important has been orienting myself and figuring out where everything is located.  Decks are labeled from ‘A’, the lowest, to ‘G’, the uppermost deck area. My quarters are on the ‘E’ deck.  The Galley, where food is prepared and served, is on the ‘D’ deck below me, and the Bridge (steering and control of the ship) is above me on the ‘F’ deck.

I have my own room—kind of luxurious living!  There’s a bunk, the head (bathroom), a couple of closets, drawers, and even a small fold-down desk area so that I can write my journals.  Every drawer latches tightly to minimize the chance of unidentified flying objects if we hit some rough weather.

Home, sweet home.
Home, sweet home.

I took a short tour of some of the more esoteric parts of the ship, including a visit to the cofferdam, whose access was through a hatch and down a ladder hidden in one of the heads (bathrooms).  This is sort of like accessing the crawl space under your house through a small tunnel in your bathroom.  While we speculated on just what purpose this area served (storage, poor planning in designing the hull and layout, a random skinny place to hang out?), it turns out that it is a watertight compartment that separates the contact between liquids that might be in the bow area and those in the stern area of the ship.

Starla Robinson leads us down the hatch into the cofferdam
Starla Robinson leads us down the hatch into the cofferdam
Lt. Quintero in the cofferdam.
Lt. Quintero in the cofferdam.

There was also an escape hatch that was incredibly heavy to lift—but I am sure you could lift it if your life depended on it!  I don’t plan on having to test this thing out!!

Just in case you need to get out in a hurry!
Just in case you need to get out in a hurry! 

Louise Todd: Ready to Go! September 9, 2013

NOAA Teacher at Sea
Louise Todd
Soon to be Aboard NOAA Ship Oregon II
September 13 – 29, 2013

Mission: Shark and Red Snapper Bottom Longline Survey
Geographical Area of Cruise: Gulf of Mexico
Date: September 9, 2013

Welcome to my NOAA Teacher at Sea Blog!

Personal Log

Sea Pork
On Jekyll Island, GA with a Sea Pork

I am thrilled that in just a few days I will be aboard NOAA ShipOregon II as a NOAA Teacher at Sea.  I have been eagerly waiting for this week to arrive and now it is almost here!  On Friday, September 13, I will fly from New Orleans to Houston and then drive to Galveston.  I will be aboard the Oregon II from Galveston, Texas until we dock in Pascagoula, Mississippi on September 29.

I am the Education Coordinator at the Audubon Aquarium of the Americas in New Orleans, Louisiana.  I manage our education animal collection, those animals that are used in programs at the aquarium and in our outreach programs, and I coordinate the AquaKid program.  Our animal collection includes a range of animals from saltwater invertebrates like horseshoe crabs to large reptiles like a red tail boa.  Caring for these animals is one of the best parts of my job.  I love interacting with them each day and ensuring they receive quality care.  Our program animals are an important part of our mission to connect our audiences to nature.  Inviting our guests to interact with these animal ambassadors helps demonstrate just how awesome animals can be!  The AquaKids are youth volunteers who enter our program when they are in 7th-9th grades.  AquaKids go through a training session during the month of July that covers basic marine biology and prepares them to serve as educators at the Aquarium for the next school year.  Some of my favorite parts of the summer training session with the AquaKids are the field trips we take every week and the dissection of spiny dogfish that we do in the last week of training.  I am ecstatic to be aboard the Oregon II and to be able to bring back new research and information to share with the AquaKids during our summer training.

Shark Disection
AquaKids dissecting a spiny dogfish
Audubon Youth Volunteers at the Sorting Table
Audubon Youth Volunteers at the sorting table on a summer field trip

Science and Technology Log

I will be aboard the Oregon II participating in the fourth and final leg of a shark and red snapper longline survey.  These longline surveys are crucial in assessing the populations of sharks and red snapper in the Gulf of Mexico and the western Atlantic Ocean.  You will be able to track the progress of the Oregon II as we move through the Gulf of Mexico using NOAA’s ship tracker.  I will be participating as a member of the science crew working a 12 hour shift each day.  I cannot wait to see what we catch during this leg of the survey!  This will be an amazing opportunity for me to see population research in action and to share that research with my blog readers and visitors to the Audubon Aquarium when I return from this experience.

I have had a great summer with trips to the barrier islands of Georgia for vacation and New York for my sister’s wedding.  This time aboard the Oregon II will be an exciting end to my summer.  I hope you will continue reading as I post about my experience and ask any  questions you might have in the comments section!

Susy Ellison: How Long Does it Take to Get to Kodiak, Alaska? September 7, 2013

NOAA Teacher at Sea
Susy Ellison
Aboard NOAA Ship Rainier
September 9-26, 2013

Mission:  Hydrographic Survey
Geographic Area: South Alaska Peninsula and Shumagin Islands
Date:  September 7, 2013

Weather:
Partly cloudy at the Anchorage Airport
Lat 61.217 N, Lon 149.900 W
Temp 56F

Personal Log

Although Mapquest says ‘you can’t get there from here’, when queried about routes from Carbondale, CO to Kodiak, AK, I am sitting in the Anchorage Airport and well on my way to meeting up with the NOAA Ship Rainier.  While it’s easy to make a list of exactly how I’m getting to Kodiak (drive to Vail, CO, shuttle van to Denver, fly from Denver to Seattle, Seattle to Anchorage, and Anchorage to Kodiak), it’s a little more complicated to actually describe my journey to Kodiak and the Rainier.

 

Sitting in Vail waiting for the shuttle van to Denver.
Sitting in Vail waiting for the shuttle van to Denver.

I’m not sure that the journey only started when I packed my large, orange duffel bag and threw it in the car.  That bag, currently either in the underbelly of a plane or sitting in a stack somewhere in the bowels of the airport, is filled with the clothing and personal supplies I’ll need for the next 3 weeks.  Topping the list of clothing is a pair of Xtratuffs–rubber boots to keep my feet dry on the ship and when we’re on shore.  Speaking of dry, I have 2 sets of raingear; a gore-tex parka and pants for those mostly wet days, and pvc-coated nylon parka and pants for the truly wet days.  Rumor has it that it could be a bit rainy in the Shumagin Island area.  I have long underwear to keep me warm, a wool hat to keep my head toasty, and the usual assortment of jeans and t-shirts for time ‘indoors’ on the ship.

Sometimes I think this journey started while planning 3 weeks of lesson plans for my students. My mind was already on the ship as I was creating those plans and trying to link my students’ activities with some of what I will be learning during my cruise.  I created an independent study plan for students who wanted to earn science credit by following along with my blogs and reading the blogs of other teachers.  All that planning gave me ample time to think about the journey that lay ahead, and to, perhaps, already start the journey while I was sitting at my desk.

This journey to Kodiak and the Shumagin Islands certainly has some foundation in my endless perusal of the Teacher at Sea blogs this summer.  I was an avid reader of blogs from teachers aboard the Rainier, but also took time to read journals from teachers in other oceans and locations.  Since I’ve never been on a ship this was a great way to start my trip a little bit ‘early’.

Did this journey begin way back when I applied for the Teacher at Sea program?  After all, part of the application process involved envisioning how I would use this experience in my classroom.  I had been following other teacher’s cruises for many years, so it was great to have to visualize myself on a ship and what I could learn from such an experience.

But, when I really think about this journey, it might actually have started long ago, when I was a child.  I was lucky enough to grow up in a household that was, to put it mildly, firmly rooted in science and looking at the world as one giant science experiment.  I was taught to ‘think like a scientist’, observing the world around me and asking questions (and searching for answers) about our planet.

It comes down to a question of scale.  Is it really just a journey of 3000+ miles from Carbondale to Kodiak, or is it the sum total of days, months, or even years?  Either way, I can’t wait for this part of the journey to end and my life on the ship to begin!

Britta Culbertson: Hiding Out During Rough Seas, September 6, 2013

NOAA Teacher at Sea
Britta Culbertson
Aboard NOAA Ship Oscar Dyson
September 4-19, 2013

Mission: Juvenile Walley Pollock and Forage Fish Survey
Geographical Area of Cruise: Gulf of Alaska
Date: Friday, September 6th, 2013

Weather Data from the Bridge (for Sept 6th at 5:57 PM UTC):
Wind Speed: 42.65 knots
Air Temperature: 11.8 degrees C
Relative Humidity: 81%
Barometric Pressure: 987.4 mb
Latitude:57.67 N          Longitude: 153.87 W

Science and Technology Log

Weather Advsisory
The weather advisory for the Gulf of Alaska and around Kodiak Island (screen shot from NOAA Alaska Region Headquarters)
Spiridon Bay
Spiridon Bay (screenshot from Shiptracker.noaa.gov)

As you can see from my weather data section, the wind speed this morning was up to 42.65 knots.  We had waves near 18 feet and thus the Oscar Dyson ran for cover and tucked itself in an inlet on the North side of Kodiak Island called Spiridon Bay.  The Oscar Dyson’s location can be viewed in near real-time using NOAA’s Shiptracker website.   The screenshot above was taken from the Shiptracker website when we were hiding from the weather. The weather forecast from NOAA’s Alaska Region Headquarters shows that the winds should diminish over the next few days.  I’m thankful to hear that!

…GALE WARNING TONIGHT….TONIGHT…S WIND 45 KT DIMINISHING TO 35 KT TOWARDS MORNING. SEAS 23FT. PATCHY FOG..SAT…SW WIND 30 KT DIMINISHING TO 20 KT IN THE AFTERNOON. SEAS15 FT. PATCHY FOG..SAT NIGHT…W WIND 15 TO 25 KT. SEAS 8 FT. RAIN..SUN…SW WIND 20 KT. SEAS 8 FT..SUN NIGHT…S WIND 25 KT. SEAS 8 FT..MON…SE WIND 25 KT. SEAS 13 FT..TUE…S WIND 30 KT. SEAS 11 FT..WED…S WIND 25 KT. SEAS 9 FT.

Since the Dyson has been in safe harbor in Spiridon Bay for the last few hours, I have had some time to catch up on some blogging!  Let’s backtrack a few days to Wednesday, September 4th, when the Dyson left Kodiak to begin its journey in the Gulf of Alaska.  We headed out after 1PM to pick up where the last cruise left off in the research grid.  We reached our first station later in the afternoon and began work.  A station is a pre-determined location where we complete two of our surveys (see map below).  The circles on the map represent a station location in the survey grid.  The solid circles are from leg 1 of the cruise that took place in August and the hollow circles represent leg 2 of the cruise, which is the leg on which I am sailing.

The first step once we reach a station is to deploy a Bongo net to collect marine zooplankton and the second step is to begin trawling with an anchovy net to capture small, pelagic juvenile pollock and forage fishes that are part of the main study for this cruise. Pelagic fish live near the surface of the water or in the water column, but not near the bottom or close to the shore.  Zooplankton are “animal plankton”.  The generic definition of plankton is: small, floating or somewhat motile (able to move on their own) organisms that live in a body of water. Some zooplankton are the larval (beginning) stages of crabs, worms, or shellfish.  Other types of zooplankton stay in the planktonic stage for the entirety of their lives. In other words, they don’t “grow up” to become something like a shrimp or crab.

Station Map
Station map for leg 1 and leg 2 of the juvenile pollock survey. I am on leg 2 of the survey, which is represented with hollow circles on the map.

Before we reached the first station, we conducted a few safety drills.  The first was a fire drill and the second was an abandon ship drill.  The purpose of these drills is to make sure we understand where to go (muster) in case of an emergency.   For the abandon ship drill, we had to grab our survival suits and life preservers and muster on the back deck.  The life rafts are stored one deck above and would be lowered to the fantail (rear deck of the ship) in the event of an actual emergency.  After the drill I had to test out my survival suit to make sure I knew how to put it on correctly.

Life Jacket
Britta Mustering for Abandon Ship Drill on Oscar Dyson
survival suit
Britta models a survival suit – they even found a size SMALL for me!

On the way to our first station, we traveled through Whale Pass next to Whale Island, which lies off of the northern end of Kodiak Island.  While passing through this area, we saw a total of 4 whales spouting and so many sea otters, I lost track after I counted 20.  Unfortunately, none of my pictures really captured the moment.  The boat was moving too fast to get the sea otters before they flipped over or were out of sight.

Whale Island
A nautical chart map for Whale Island and Whale Passage

Personal Log

secure for sea!
Last night’s warning about high seas in the early morning of September 6th.

A lot of people have emailed to ask me if I have been getting seasick.  So far, things haven’t been that bad, but I figured out that I feel pretty fine when I’m working and moving about the ship.  However, when I sit and type at a computer and focus my attention on the screen that seems to be when the seasickness hits. For the most part, getting some fresh air and eating dried ginger has saved me from getting sick and fortunately, I knew about the threat of high winds last night, so I made sure to take some seasickness medication before going to bed.  After what we experienced this morning, I am sure glad I took some medication.

Everyone on board seems very friendly and always asks how I am doing.  It has been a real pleasure to meet the engineers, fisherman, NOAA Corps officers, scientists, and all others aboard the ship.  Since we have to work with the crew to get our research done, it’s wonderful to have a positive relationship with the various crew members.  Plus, I’m learning a lot about what kinds of careers one can have aboard a ship, in addition to being a scientist.

So far, I’ve worked two 12-hour shifts and even though I’m pretty tired after my long travel day and the adjustment from the Eastern Time Zone to the Alaskan Time Zone (a four hour difference), I’m having a great time!  I really enjoy getting my hands dirty (or fishy) and processing the fish that we bring in from the trawl net.  Processing the haul involves identifying, sorting, counting, measuring the length, and freezing some of the catch.  The catch is mainly composed of different types of fish like pollock and eulachon, but sometimes there are squid, shrimp, and jellyfish as well.

One of the hardest parts of the trip so far is getting used to starting work at noon and working until midnight.  We have predetermined lunch and dinner times, 11:30 AM and 5:00 PM respectively, so I basically eat lunch for breakfast and dinner for lunch and then I snack a little before I go to bed after my shift ends at midnight.  As the days go by, I’m sure I’ll get more used to the schedule.

Did You Know?

During one of our trawls, we found a lanternfish.  Lanternfish have rows of photophores along the length of their bodies.  Photophores produce bioluminescence and are used for signaling in deep, dark waters.  The fish can control the amount of light that the photophores produce.  Lanternfish belong to the Family Myctophidae and are “one of the most abundant and diverse of all oceanic fish families” (NOAA Ocean Explorer).

lanternfish
Lanternfish caught during a trawl. Note the dots along the bottom of the fish, these are photophores that emit bioluminescence.

Lanternfish
Photo of bioluminescing lanternfish (Photo Credit: BBC Animal Facts http://www.bbc.co.uk/nature/blueplanet/factfiles/fish/lanternfish_bg.shtml)