Susan Brown: Let’s Go Fishing, September 4, 2017

 

NOAA Teacher at Sea

Susan Brown

NOAA Ship Oregon II

September 3 – 15, 2017

Mission: Snapper/Longline Shark Survey

Geographic Area of Cruise: Gulf of Mexico

Date: September 4, 2017

Weather Data from the Bridge

Latitude: 29 43.931N
Longitude: 086 09.617W
Sea wave height: .5 meters
Wind Speed: 2
Wind Direction: 250 degrees
Visibility: good
Air Temperature: 28.3 degrees Celsius
Barometric Pressure: 1016 mb
Sky: partly cloudy

Science and Technology Log

Numbered tags used for each hook
Mackerel used for bait

Today was my first shift. We are using mackerel to bait the 100 hooks that will be places into the water at a specific station. Each hook is numbered so that we can collect data on which hook brought in a fish and entered into the database. There are several jobs out here from baiting the hooks, placing the buoys, flinging the baited hooks out, and recording data in the computer. My job today is the computer.

entering data on the deployment of the baited hooks

The longline is set and left to sit in the ocean for approximately one hour before we start bringing up the line to see if we have a fish on. Out of the 100 hooks we got one fish, a baby tiger shark and a larger juvenile tiger shark coming in at six feet or so. This tiger shark had several hooks in its mouth as well as a tag so when she was brought up on board, all the hooks were removed and the tag replaced with a new one.

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Removing hooks from the tiger shark’s mouth

The tag that was on the tiger shark was opened up to reveal a small scroll of paper with a unique number so that this shark can be tracked from where it was first picked up to when it ended up with us for the brief visit. Below is a short video of us bringing up the shark in the cradle! [no dialogue or narration.]

We will be setting another line tonight at our second station as we continue to motor southeast following the coast of Florida.

Beside recording data on the sharks, a CTD is deployed to collect data on conductivity, temperature and depth. We will use this data in the classroom to look for trends between the abiotic factors that may influence where we are finding certain shark species and the number of overall sharks at any given station.

The CTD that measure conductivity, temperature and depth

Personal Log

There are many different scientists on board researching different things. I am sharing a stateroom with Dani who is on the night shift. She is looking into how different sharks handle stress. I see very little of her since we are on opposite shifts so we get a quick visit at noon when there is a changing of the guards so of say. Brett and Carlos, as mentioned in an earlier post, are looking into parasites that inhabit the various animals we are bringing up. I will do a separate blog on those two and their research later this week to share what they are finding.

Donning the survival suit during abandon ship drill

Today we had a few drills to practice in case of an emergency. One was a fire drill and the other was an abandon ship drill where I had to don a large neoprene suit in less than two minutes. Here I am in that suit! It was quite cumbersome to put on.

Learning new words as I get acclimated to the ship. Here are a few for you:

The head = bathroom

Stateroom = room where I sleep

Muster = to assemble

Bow = the front of the ship

Stern = the back of the ship

Did You Know?

Military time is used on board this ship. See the photo of the clock below.

Question of the Day: Why use military time?

NOAA clock

Susan Brown: Getting Acclimated, September 3, 2017

NOAA Teacher at Sea

Susan Brown

Aboard NOAA Ship Oregon II

September 2 – 15, 2017

Mission: Shark/Red Snapper Longline Survey
Geographic Area of Cruise: Gulf of Mexico
Date: September 3, 2017
Weather Data from the Bridge

Latitude: 30degree06.7N
Longitude: 88degree17.6W
Sea wave height: <1
Wind Speed: LT
Wind Direction: VAR
Visibility: 10NM
Air Temperature:
Barometric Pressure:
Sky: BKN

Incomplete weather data as we were docked.

I’m currently sitting on the Oregon II docked in Pascagoula, Mississippi after a long travel day. It’s eerily quiet as the ship disembarks tomorrow at 14:00 and the majority of the crew will arrive tomorrow. I am enjoying the slow introduction to this ship and finding my way around. The OOD (Officer Of the Deck) gave me a tour of the ship that I will be working on for the next two weeks. The majority of crew is on shore for the Labor Day weekend but will return tomorrow as we disembark and head towards Florida. Our plans have changed due to Hurricane Harvey and debris that may be in the waters making the travel in those waters unsafe.

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NOAA Ship Oregon II in dock

Science and Technology Log

Due to Hurricane Harvey, the area being surveyed has changed so that we are heading East instead of West to pick up the third leg of this survey that ended off the coast of Florida last week. I have been assigned the day shift from noon to midnight and will be assisting the science crew. The mission of this survey is to monitor interannual variability of shark populations of the Atlantic coast and the Gulf of Mexico. Additionally aboard are two scientist that are on board are studying parasites that these animals carry. Carlos and Brett, the two parasitologists, were on the second leg right before I joined. Their leg started on the tip of Florida and ended where we will start.

Personal Log

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Wearing “the patch” to keep from getting seasick

Seasick? Felt a little queasy after my first night in dock! Decided the best course of action was to take some medicine, eat a big meal and hydrate to help get my sea legs. Everyone has been friendly and welcoming as we get started. The night crew starts tonight at midnight till noon and the day crew, where I am been placed, will start at noon. Hoping for a good night’s sleep!

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My bed is the bottom one!

Did You Know?

Sharks have been around since the dinosaurs approximately 450 million years ago.

Question of the day

What is NOAA’s mission statement? (Hint: Google NOAA and select “About Our Agency” at the bottom)

Amanda Dice: From Fin to Wing, September 1, 2017

NOAA Teacher at Sea

Amanda Dice

Aboard Oscar Dyson

August 21 – September 2, 2017

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We have made it around Kodiak Island and will dock in Kodiak tomorrow morning.

Mission: Juvenile Pollock Fishery Survey

Geographic area of cruise: Western Gulf of Alaska

Date: September 1, 2017

Weather Data: 12 C, sunny

Latitude: 57 40.9 N, Longitude: 151 37.2 W

 

 

Science and Technology Log

In addition to NOAA’s juvenile walleye pollock survey, this leg of voyage is also hosting a seabird survey. The United States Fish and Wildlife Service (USFWS) sent a scientist aboard Oscar Dyson to identify and record bird species as the boat travels from one sampling station to the next. To do this, a bird observation station has been set up on the port side (left hand side) of the bridge. This is a good spot to get a clear view of the water and sky ahead of the boat and to the port side.

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Jessica “the bird lady” keeps a sharp eye out for birds from her station on the bridge.

Not every bird that is seen from the bridge is included. There are some guidelines that must be followed in order to collect data that has scientific validity. One of the major guidelines is that the ship should be moving at a consistent speed for each of the observation periods. If a scientist were to observe birds at a slower speed, he or she might end up recording more species because there is more time to look for and identify then. If a scientist were to observe birds at a faster speed, he or she might end up recording fewer species because there is less time to look for them and identify them.

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A northern fulmar soars alongside the ship.

It is difficult to correctly identify birds at a distance further than 300 meters away. It is also much more likely that a bird will be identified correctly if it closer than if it is further away. In order to account for differences in how accurately a bird can be identified, scientists have set up a system to put the data collected into different categories. First of all, only birds that are 300 meters away or closer are counted and identified. Birds that are seen between 0 – 50 meters away are considered in “Bin 1” and can be identified with the most accuracy. Bin 2 is 50 – 100 meters away, Bin 3 is 100 – 200 meters away, and Bin 4 is 200 -300 meters away. The further away a bird is, the greater the chance that it will not be identified correctly or missed altogether.

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This diagram shows how birds are categorized into bins depending on how far away they are when they are spotted.

Some of the common birds seen on this survey in the Gulf of Alaska include northern fulmars, auklets, shearwaters, black-footed albatross, tufted and horned puffins, storm petrels, kittiwakes, and common murres. Some of these birds, like the fulmars and albatross like to hang around the boat and look for an easy meal from the fishing net. This can make it difficult to avoid counting the same bird more than once. Adjustments are made by the scientist to prevent an overestimation in the number of birds recorded.

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A pair of albatross looks for food off of the starboard (right) side of the ship.

We have also seen some very unexpected bird species. There was a trio of peregrine falcons that landed on the ship and traveled with us for a day. Some of the crew on the bridge saw one of them catch a smaller bird and fly off with it! There was also a masked booby that spent a few hours cruising along with us. Masked boobies are native to the waters much further south and have never been seen in the Gulf of Alaska!

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A masked booby is far from home. Photo by Jessica Stocking
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One of three peregrine falcons spends the day perching on different spots of the Oscar Dyson. Photo by Jessica Stocking

Other data about the weather conditions are automatically recorded with the help of a computer. Air temperature, water temperature, wind speed, and wind direction are recorded at the start of each observation session. A GPS device also records the latitude and longitude of the ship every few seconds. All this information helps scientists get a better understanding of which birds were present at different times of year and how weather conditions may affect where they go.

 

DLOG screen capture
GPS, weather, and bird species data are collected in one spot.

Personal log

This is the last day of the survey and it is finally sunny! It has been an interesting two weeks for me. It was full of observing new animals and gaining a new understanding of how marine science is conducted. It has also been a great opportunity to meet some very interesting people passionate about their work.

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My roommate, Jessica, and I in our stateroom bunks.

 

Did you know?

Flatfish have one eye that migrates, or moves, from one side of their head to the other! This happens within the first few months after they hatch. The result is that both of their eyes end up on the same side of their head. This allows flatfish to swim along the bottom of the ocean floor while keeping both eyes facing upward to look for food and to spot predators.

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These two flatfish are a few months old. They already have both eyes on one side of their head.

Chelsea O’Connell-Barlow: Full Steam Ahead, August 30, 2017

NOAA Teacher at Sea

Chelsea O’Connell-Barlow

Aboard NOAA Ship Bell M. Shimada

August 29 – September 12, 2017

 

Mission: Pacific Hake Survey

Geographic Area of Cruise: NW Pacific Ocean

Date: 8/30/2017

 

Weather Data from the Bridge:

Latitude: 48.472837N

Longitude: -124.676694W

Temperature 59 F

Wind 9.7 knots

Waves 3-5 feet

Science and Technology Log

We have not started fishing yet because we are heading to our first transect off the western coast of the Haida Gwaii archipelago. I thought this would be a perfect time to introduce another research project that is gathering data on the Shimada. One of my roommates, Lynne Scamman, is on-board researching Hazardous Algal Blooms (HABs).

Lynne in Chem lab
Lynne Scamman running wet chemistry tests and identifying phytoplankton.
  1. What are Hazardous Algal Blooms?

They are large numbers of phytoplankton, either diatoms or dinoflagellates, who produce toxins. Phytoplankton are essential to the ecosystem because they produce half of the global oxygen. However under certain circumstances these organisms reproduce rapidly, skyrocketing the population, this is a bloom. Some of these phytoplankton produce toxins. When the populations are low the toxins aren’t a big deal. However, when a bloom of phytoplankton that produce toxins occurs there can be health concerns for organisms exposed to the toxins. We have to consider the marine food chain and something called bioaccumulation. Phytoplankton along with zooplankton create the base of the marine food web. Organisms who eat toxin producing phytoplankton retain the toxin in their body. Then any organism who eats them will also hold that toxin. You can see how the toxin would accumulate along the food chain and potentially hold serious side effects for organisms with high levels of toxin.

  1. Why is research being done on HABs?

HABs are becoming a problem for humans along the coasts and in the Great Lakes. Basically all of the factors that contribute to the increase in HABs are a product of human impact. Global climate change, increased nutrient pollution and global sea trade are all factors contributing to the rise in Hazardous Algal Blooms. We want to monitor so that eventually we will be able to predict when, where and why the HABs will occur.

  1. Why are YOU studying HABs?

One day I walked into my college biology lab and met a guest instructor who specializes in all things phytoplankton related. I was blown away by the complexity that some of these single celled organisms held. The professor shared a few species names and I started investigating. The species that grabbed my attention is called Nematadinium armatum. This organism has a rudimentary eye called a melanosome and nematocysts for hunting, again this is pretty impressive for an organism made of one cell. Once I learned about the variety in this microscopic world and how influential they were to the health of the entire ocean, I knew that I wanted to learn more.

Personal Log

I am still figuratively pinching myself every few hours at just how amazing this experience is to participate in first hand. Yesterday we left the dock of Port Angeles at 10am and the boat hasn’t slowed down since. We did drills to ensure that all aboard knew where to go in case of fire and if we needed to abandon ship. Part of the abandon ship drill is to make sure that everyone has and can get into their Immersion Suit aka “Gumby Suit.” This suit is amazing! This portion of the Pacific is quite cold and the Immersion suit would keep you warm and buoyant until a rescue can occur.

OCB Gumby
Trying on the Immersion suit.

After our drills several of the science crew went up to the Flying Bridge to look for marine mammals. We were cruising between Cape Flattery, Washington and Vancouver Island, British Columbia with high hopes of seeing activity. WOW, we lucked out. We spotted 17 Humpback whales, 2 Harbor porpoise and 2 Dall’s porpoise. We are also seeing several types of sea birds but I am still brushing up with the Sibley to id birds from this area.

Shimada Flags
The Shimada under two flags as it enters Canadian waters.

 

Did You Know?

The island cluster that we are heading to had a name change at the end of 2009. What was formerly called Queen Charlotte Islands is now called Haida Gwaii. This name change came as part of a historic reconciliation between British Columbia and Haida nation. Haida Gwaii translated means “island of the people.”

Haida Gawaii
Map of Haida Gawaii area.

Lisa Battig: Nome, Alaska & Launch 2808, August 30, 2017

NOAA Teacher at Sea

Lisa Battig

Aboard NOAA Ship Fairweather

August 28 – September 8, 2017

 

Mission: Hydrographic Survey leg IV

Geographic Area of Cruise: Alaska

Date: Wednesday, August 30, 2017
Location: Port Clarence: 65o14.034N 166o43.072W

Weather on the bridge:
30+ knot winds, 42o F, 4ft seas, heavy stratocumulus clouds (9/10 coverage)

Science & Technology Log

Over the past two days I have been introduced to tremendous amounts of the science of hydrography. In this blog post I will focus on the hardware used and the process of surveying. There are two types of sonar that are being employed. The first is side scan sonar and the second is multibeam sonar.

Side Scan
Side scan array sonar housed underneath one of the small launch vessels

 

Side scan is shorter range and performs better in shallower water. Side scan is used in conjunction with multibeam, however, as side scan does not give true depth values. The function of side scan is to show features evident on the ocean floor. For this reason, multibeam is run in conjunction with side scan in order to keep an accurate record of depths.

Multibeam
Multibeam sonar housed underneath another of the small launch vessels

Multibeam shows an exact depth. Due to the fact that it is an angular spreading band from the center of the underside of the launch, at shallow depths it will only show a very narrow strip of ocean floor.


Stop and imagine…a lit flashlight shining on a wall from only a few centimeters away. What happens to the image on the wall as you pull the flashlight back? The area of coverage of the image will become larger. The concept is similar for the multibeam in shallow versus deeper water.


Using multibeam in shallow water then would create a need for more passes closer together in order to cover an area. There are instances where using this technology even in shallow water would make sense, but for a full coverage survey, this would not be the case.

CTD Image 2
A CTD; it contains sensors for conductivity, temperature and density of the water column

The third piece of hardware used for the standard small boat launch hydrographic surveys is the CTD device. The CTD will measure conductivity of the water and also give both a temperature and density profile. The CTD is deployed multiple times during a survey as a tool to calibrate the data that is coming in via the sonar. Conductivity of the water gives an estimate of the total dissolved solids in the water. This information, along with the temperature and density will give an estimate of sound speed through the water column.


Stop and try this one for better understanding… knock on a door normally with your head roughly arm’s distance from the point where you are knocking. Now repeat the process of knocking, but with your ear pressed against the door approximately an arm’s length away from the knock. What is different? You should have noticed that a more precise (and typically louder) sound reached your ear. If you pay close attention, you will also notice that the sound reaches your ear more quickly. This is roughly analogous to how changes in the water column will affect sound speed.


The final piece of equipment used regularly for surveys is a HorCon (horizontal control) station. This is a land-based station that will help to define accurate position in the water. It allows for greater precision with global positioning data. The signals of satellites responsible for global position are affected daily by changing atmospheric conditions. Moreover, the precise positions of the satellites themselves are actually not well known in advance. This may result in a GPS location moving a few centimeters in one direction or another. While this is not going to heavily impact your ability to find a Starbucks in a strip mall, it can have a definite impact on the accuracy of charts for navigation. The HorCon station always remains in the same place on land, and can therefore be used to calibrate the measurements being read in the survey waters nearby and that information can be used along with corrected satellite positions since it is coming after the fact.

Port Clarence chart
A nautical chart of the Port Clarence and Grantley Harbor area where we were surveying

Today we worked in Port Clarence, Alaska, both outside and inside of Grantley Harbor. Most of the depths being surveyed are in the 4-6 meter range. The particular area being surveyed had been previously surveyed in the 1950s by the US Coast and Geodetic Survey, likely using a single beam sonar system. The current survey is intended to note changes that have occurred since that prior survey and to accurately update all of the charts. The area of western Alaska is expected to increase in boat traffic over the coming years due to the opening of the Northwest Passage from the Pacific to the Atlantic via the Arctic. This route is significantly shorter for most shipping traffic than the route through the Panama Canal. Because of this expected increase in traffic, there is a need to identify areas for sheltering during heavy seas. Port Clarence is a natural inlet that offers some protection and holds potential for this purpose.

The process of surveying:
Two launches were deployed. I was on launch 2808, the second described here. The first was equipped with only multibeam sonar and the second had both multibeam and side scan. The plans for the two launches were different. The launch with only multibeam was working in an area of Grantley Harbor and covering an area that had previously been mapped to insure that the values were acceptably accurate. This focus existed primarily because of extra time available up in this area. The launch running the side scan was completing some unfinished work in Port Clarence and then did further work inside of Grantley Harbor. These areas, or “sheets” are described below. As a side note, small boat deployment is a fascinating and involved activity that I will discuss in a later blog.

Survey areas are broken up into sections known as “sheets” – each sheet has a manager. This person will be from either the NOAA Corps or a civilian member of the scientific survey team. The sheet manager will be responsible for setting up the plan for survey and doing all of the final checks after data has been gathered, cleaned and examined to determine if there are areas that should be rechecked or run again before it is completed and undergoes final processing.

A sheet manager will need to consider several questions prior to setting up the initial parameters for the survey. What is the depth being surveyed? What type of bottom is it? What type of coverage is needed? All of these factors will come into play when determining how the lines will be run – how long, how far apart, which sonar type, etc.
Once the plan is determined, it will be the job of the Operations Officer, LT Damian Manda, to parse out the duties and create a daily work plan to cover all of the areas. Each day, multiple launches will be sent out to gather data as described above. As the fieldwork finishes for the day, data will be transferred to a drive and then brought into the ship’s mapping room where night processers will begin the lengthy work of checking and cleaning the data so that it can all be ready for the final processing step prior to being sent to the client.

HMarshburn at computer
Senior surveyor Hannah Marshburn at the computer terminal in launch 2808

How good are those data?
There are several checks built into the data collection process. First, the survey team members on the launches are watching in real time. With three screens to work from, they are able to see what the sonars are seeing and can also set certain limits for the data that will alarm when something appears to be contrary to what’s expected. Night processors look for anomalies in the data like sudden inexplicable drops in depth in an otherwise flat surface or an extremely “noisy” area with little good data. Any area with a former survey will also be compared to the previous values with large differences signaling possible issues. Many trained eyes look at the data before it is accepted for charting and there will commonly be at least one return to an area to check and recheck prior to completion. One area in the current survey has continued to show odd results, so trained NOAA divers will dive the area to find out what is really going on.

Personal Log

So far this has been an amazing experience. I fully enjoy being among the crew of the Fairweather and living on the ship. It’s hard to say what my favorite part has been so far because I have honestly enjoyed all of it! Since we didn’t get underway until Monday, I had the opportunity on Sunday to roam around Nome with a couple of the other folks that are just here for two weeks, LT Joe Phillips and LCDR Ryan Toliver. I learned a lot more about both the NOAA Corps and the Public Health Service of which they are respectively a part. (These are two of the seven uniformed services – can you name the other five?) NOAA Corps officers are in command on all of the active NOAA commissioned ships and aircraft and you will learn a lot more about them in future posts. The PHS is an organization made up primarily of medical professionals. These folks serve in various medical and medical research positions around the nation. There are many who will work for the National Institutes of Health in research, or the Bureau of Prisons or commissioned vessels like Fairweather as practitioners. Unlike NOAA Corps, PHS is not on a billet cycle where every two to three years you will be moved to a new position in a different office or location. Similar to all of the other uniformed services, though, promotion through the ranks is both encouraged and desired.

Traditional Boat - Nome
As we walked all around Nome, this was one of the sights – the frame of a traditional fishing boat.

We also saw the marker for the end of the Iditarod race. I was able to see the historic beginning in Seward, Alaska back in 2010, so seeing the end in Nome was an unexpected treat. Nome also has Cold War-era missile early warning system arrays at the top of a mountain nearby. We had a chance to hike around them and see some of the interesting geologic features of the area. There’s so much more to talk about, but I think I’ll stop here and save shipboard life for my next post.

Did You Know…

… that the Iditarod has its historic beginnings with the Public Health Service? There were many children in interior and western Alaska dying of diphtheria in the early 1920s. When it reached epidemic proportions, the only doctor in Nome reached out to the PHS in the lower 48 to ask for help. Vials of serum were found and sent north to Seward, but then because of heavy ice and storming, dog sled teams were used to get the vials to the interior towns and to Nome. The original race along the Iditarod Trail was run as a memorial to the “Serum Run” and eventually evolved into the highly competitive race it is today.