currents – NOAA Teacher at Sea Blog

June 23, 2013August 11, 2021

Sue Cullumber: Drifting Away, June 21, 2013

NOAA Teacher at Sea
Sue Cullumber
Onboard NOAA Ship Gordon Gunter
June 5–24, 2013

Mission: Ecosystem Monitoring Survey
Date: 6/21/2013
Geographical area of cruise: The continental shelf from north of Cape Hatteras, NC, including Georges Bank and the Gulf of Maine, to the Nova Scotia Shelf

Weather Data from the Bridge: Time: 21.00 (9 pm)
Latitude/longitude: 3734.171ºN, 7507.538ºW
Temperature: 20.1ºC
Barrometer: 1023.73 mb
Speed: 9.6 knots

Getting ready to launch the buoy – photo by Chris Taylor.

launchingdrifter — Launching the buoy from the ship’s stern – photo by Chris Taylor.

Science and Technology Log:

This week we launched a Global Drifter Buoy (GDB) from the stern of the Gordon Gunter. So what is a GDB? Basically it is a satellite tracked surface drifter buoy. The drifter consists of a surface buoy, about the size of a beach ball, a drogue, which acts like a sea anchor and is attached underwater to the buoy by a 15 meter long tether.

Drifter tracking: The drifter has a transmitter that sends data to passing satellites which provides the latitude/longitude of the drifter’s location. The location is determined from 16-20 satellite fixes per day. The surface buoy contains 4 to 5 battery packs that each have 7-9 alkaline D-cell batteries, a transmitter, a thermistor to measure sea surface temperature, and some even have other instruments to measure barometric pressure, wind speed and direction, salinity, and/or ocean color. It also has a submergence sensor to verify the drogue’s presence. Since the drogue is centered 15 meters underwater it is able to measure mixed layer currents in the upper ocean. The drifter has a battery life of about 400 days before ending transmission.

decoratingdrifter — Attaching the stickers to the buoy – photo by Kris Winiarski.

Students at the Howard Gray School in Scottsdale, Arizona designed stickers that were used to decorate the buoy. The stickers have messages about the school, Arizona and NOAA so that if the buoy is ever retrieved this will provide information on who launched it. In the upcoming year students at Howard Gray will be tracking the buoy from the satellite-based system Argos that is used to collect and process the drifter data. You can follow our drifter here, by putting in the data set for the GTS buoy with a Platform ID of 44932 and select June 19, 2013 as the initial date of the deployment.

Why are drifter buoys deployed?

In 1982 the World Climate Research Program (WCRP) determined that worldwide drifter buoys (“drifters”) would be extremely important for oceanographic and climate research. Since then drifters have been placed throughout the world’s oceans to obtain information on ocean dynamics, climate variations and meteorological conditions.

The Howard Gray School drifter on its ocean voyage.

NOAA’s Global Drifter Program (GDP) is the main part of the Global Surface Drifting Buoy Array, NOAA’s branch of the Global Ocean Observing System (GOOS). It has two main objectives:

1. Maintain a 5×5 worldwide degree array (every 5 degrees of the latitude/longitude of world’s oceans) of the 1250 satellite-tracked surface drifting buoys to maintain an accurate and globally set of on-site observations that include: mixed layer currents, sea surface temperature, atmospheric pressure, winds and salinity.

2. Provide a data processing system of this data for scientific use.

bongossunset — Bongo nets going out for the plankton samples.

meshsamples — Plankton from the different mesh sizes. The left is from the smaller mesh and contains much more sample. Photo by Paula Rychtar.

EcoMon survey: We are continuing to take plankton samples and this week we started taking two different Bongo samples at the same station. Bongo mesh size (size of the holes in the net) was changed several years ago to a smaller mesh size of .33 mm. However, they need comparison samples for the previous nets that were used and had a mesh size of about .5 mm. They had switched to the smaller net size because they felt that they were losing a large part of the plankton sample (basically plankton were able to escape through the larger holes). We are actually able to see this visually in the amount of samples that we obtain from the different sized mesh.

dolphinflying — Common Dolphins were frequent visitors to the Gordon Gunter.

Personal Log:

It’s hard to believe that my Teacher at Sea days are coming to a close. I have learned so much about life at sea, the ocean ecosystem, the importance of plankton, data collection, and the science behind it all. I will miss the people, the ocean and beautiful sunsets and the ship, but I’m ready to get back to Arizona to share my adventure with my students, friends and family. I want to thank all the people that helped me during this trip including: the scientists and NOAA personnel, the NOAA Corps and ship personnel, the bird observers and all others on the trip.

Did you know? Drifters have even been placed in many remote locations that are infrequently visited or difficult to get to through air deployment. They are invaluable tools in tracking and predicting the intensity of hurricanes, as well.

Question of the day? What information would you like to see recorded by a Global Drifter Buoy and why?

shipsunset-2 — Another beautiful sunset at sea.

May 19, 2013August 11, 2021

Emilisa Saunders: Finding the rhythm aboard the Oregon II, May18, 2013

NOAA Teacher at Sea

Emilisa Saunders

Aboard NOAA ship Oregon II

May 14, 2013 – May 30 2013

Mission: SEAMAP Spring Plankton Survey

Geographical Area of Cruise: Gulf of Mexico

Date: May 18, 2013

Weather Data: Wind Speed: 13.94 knots; Surface water temperature: 25.4; Air temperature: 26.4; Relative humidity: 87%; Barometric pressure: 1,015.33 mb

Science and Technology Log:

For the scientists on board the Oregon II, each shift follows roughly the same routine. When we start our shift, we check in at the dry lab to see how much time we have until the next sampling station. These stations are points on the map of the Gulf of Mexico; they were chosen to provide the best coverage of the Gulf waters. Our ETA, or estimated time of arrival, is determined by how fast the ship is moving, which is influenced by wind and currents, which you can see in the map below. A monitor mounted in the dry lab shows us a feed of the route mapping system that is used by the crew on the Bridge to drive the ship. This system allows us to see where we are, where we are headed, and what our ETA is for the next station. We also get warnings from the Bridge at one hour, at thirty minutes, and at ten minutes before arrival.

Gulf Currents — The currents in the Gulf of Mexico, plus our planned route. Image courtesy of NOAA.

At the 10-minute mark, we put on our protective gear – more on that later in this post – and bring the cod ends up to the bow of the boat, where we attach them to the ends of the appropriate nets. Then, we drop the Bongo nets, the regular Neuston net, the Sub-surface Neuston net, and the CTD into the water, in that order. These all go down one at a time, and each one is pulled out and the samples collected before the next net goes in.

Towing the Neuston net on the night shift

The idea of dropping a net into the water probably sounds pretty simple, but it is actually a multiple-step process that requires excellent teamwork and communication amongst several of the ship’s teams. The scientists ready the nets by attaching cod ends and making note of the data that tracks the flow of water through the net. Because the nets are large and heavy, and because of the strong pressure of the water flowing through the nets, they are lifted into the water using winches that are operated by the ship’s crew. The crew members operate the machinery, and guide the nets over the side of the ship. While this is happening, the crew members communicate by radio with the Bridge, providing them with information about the angle of the cable that is attached to the net, so that the Bridge can maintain the a speed that will keep the net at the correct angle. At the same time, a scientist in the dry lab monitors how deep the net is and communicates with the deck crew about when to raise and lower the nets. This communication takes place mostly over walkie-talkies, which means that clear and precise instructions and feedback are very important.

Operating the winches — Crewmember Reggie operating the winch, while crewmember Chris measures the angle of the cable

When each net is pulled back out of the water after roughly 5-10 minutes, we use a hose to spray any little creatures who might be clinging to the net, down into the cod end. At stations where we run the MOCNESS, we head to the stern of the ship, where the huge MOCNESS unit rests on a frame. Lowering the MOCNESS takes a strong team effort, since it is so large. After we retrieve each net, we detach the cod ends and bring them to the stern, where a station is set up for us to preserve the specimens. I’ll go into more detail about the process of preserving plankton samples in a later post.

Hosing down the nets — Alonzo, hosing down the Bongo nets before bringing them aboard.

We’ve had a couple of nights of collecting now, and so far it has been completely fascinating. I’m in awe of the variety of organisms that we’ve come across. The scientists on my shift, Glenn and Alonzo, are super knowledgeable and have been very helpful in explaining to me what we are finding in the nets. Although this is a Bluefin Tuna study, we collect and preserve any plankton that ends up in the nets, which can include copepods, myctophids, jellies, filefish larvae and eel larvae, to name a few. When we get the samples back to shore, they will be sent to a lab in Poland, where the species will be sorted and counted; then, the tuna larvae will be sent back to labs in Mississippi or Florida for further study and sometimes genetic testing.

My favorite creature find so far has been the pyrosome. While a pyrosome looks like a single, strange creature, it is actually a colony of tiny creatures called zooids that live together in a tube-shaped structure called a tunic. The tunic feels similar to cartilage, like the upper part of your ear. Pyrosomes are filter feeders, which means they draw in water from one opening, eat the phytoplankton that passes through, and push out the clean water from the other end. So far on the night shift, we’ve found two pyrosomes about four inches in length and one that was about a foot long; the day crew found one that filled two five-gallon buckets!

Alonzo and the pyrosome — Alonzo holding the pyrosome

Challenge Yourself:

Hello, Nature Exchange Traders! Pick one of the of the zooplankton listed in bold above, and research some facts about it: Where does it live? What does it eat? What eats it? Write down what you find out and bring it in to the Nature Exchange for bonus points. Be sure to tell them Emmi sent you!

Gumby Suit — In the Gumby suit, practicing the Abandon Ship drill. Photo by Glenn Zapfe

Personal Log:

Safety is the top priority on board the Oregon II. We wouldn’t be able to accomplish any of our scientific goals if people got hurt and equipment got damaged. We started our first day at sea with three safety drills: the Man Overboard drill, the Abandon Ship drill and the Escape Hatch drill. For Man Overboard, everyone on board gathered, or mustered, at specific locations; for the Science team, our location was at the stern, or back of the ship. Aft is another word for the back. From there, we all scanned the water for the imaginary person while members of the crew lowered a rescue boat into the water and circled the Oregon II to practice the rescue.

For the Abandon Ship drill, we all grabbed our floatation devices and survival suits from our staterooms and mustered toward the bow, or front of the ship. I got to practice putting on the survival suit, which is affectionately called a Gumby suit. In the unlikely event that we would ever have to abandon ship, the suit would help us float and stay relatively warm and dry; it also includes a whistle and a strobe light so that aircraft overhead can see us in the water.

For the Escape Hatch drill, we all gathered below deck where our staterooms are, and climbed a ladder, where crew members helped pull us up onto the weather deck (the area of the ship exposed to weather) on the bow of the ship. This is meant to show us how to escape dangers such as fire or flood below deck.

Safety gear on; ready for station! Photo by Glenn Zapfe

But safety isn’t just practiced during drills; it’s pretty much a way of life on the ship. Whenever winches or other machinery are in operation, we all have to wear hard hats and life jackets; that means that we wear them every time we reach a station and drop the nets. We are also all required to wear closed-toed and closed-heeled shoes at all times, unless we’re sleeping or showering. Another small safety trick that is helpful is the idea of, “keep one hand for yourself and one hand for the ship.” That means we carry gear in one hand and leave one free to hold onto the swaying ship. This has been really useful for me as I get used to the ship’s movements.

Until next time, everyone – don’t forget to track the Oregon II here: NOAA Ship Tracker

December 12, 2011August 11, 2021

Elizabeth Bullock: We Are Underway! December 11, 2011

NOAA Teacher at Sea
Elizabeth Bullock
Aboard R/V Walton Smith
December 11-15, 2011

Mission: South Florida Bimonthly Regional Survey
Geographical Area: South Florida Coast and Gulf of Mexico
Date: December 11, 2011

Weather Data from the Bridge
Time: 2:30pm
Air Temperature: 24.5 degrees C (76 degrees F)
Wind Direction: 65.9 degrees east northeast
Wind Speed: 15.8 knots
Relative Humidity: 78%

Science and Technology Log

Today is the first day of the research cruise. The R/V Walton Smith left its home port in Miami, FL this morning at about 7:30am. After a delicious breakfast, the crew and scientific party received a safety briefing from Dave, the Marine Tech. We learned about the importance of shipboard drills and we were shown the location of all the safety gear we might need in case of an emergency. This ship works like a self-contained community. The crew of the ship must also be the policemen and firemen (or policewomen and firewomen).

After our safety briefing, the science party went outside to our first station of the day. The first piece of equipment we put into the water was a CTD. The CTD is named after the three factors the equipment measures: conductivity, temperature, and depth. The CTD will be deployed at precise locations along our route. Since they conduct this research cruise twice a month, they can see if conditions are changing or staying the same over time.

Liz at computer — Here I am, reading the data that came up from the CTD.

This is the CTD, which measures conductivity, temperature, and depth.

Question for students: What is the relationship between salt and electrical conductivity? If the salt content in the water increases, will it conduct electricity better or worse?

The next piece of equipment we deployed was the Neuston Net. This net sits at the water line and skims organisms off the surface of the ocean. The net is in the water for 30 minutes at a time. After bringing the net onto the deck, the fun part starts – examining the contents! Our Neuston Net had two main species: moon jelly (Aurelia) and sargassum. The term sargassum actually describes many species, so the scientists on board will study it carefully in order to classify which kinds they caught in the net. Sargassum is an amazing thing! It is planktonic (which means that it floats with the current) and it serves as a habitat for bacteria and small organisms. Since it is such a thriving habitat, it is also a great feeding ground for many different species of fish.

Once we emptied the contents of the Neuston Net, Lindsey and Rachel, two of the scientists on board, began to measure the quantity of each species they caught. In order to measure the weight of the moon jellies, they used the displacement method. This is because we can’t use regular scales onboard. Here are the steps we took to measure the moon jellies:

1) We poured water into a graduated cylinder and recorded the water level. For example, let’s say that we poured in 100ml of water.

2) We put a moon jelly into the graduated cylinder and recorded the new water level. For example, let’s say that the new water level read 700ml.

3) We subtracted the old water level from the new, and we could tell the volume of the moon jelly we had caught. For example, based on the numbers above, we would have caught a 600ml moon jelly!

Neutson Net — Lindsey examines what we caught in the Neuston Net.

Both the CTD and the Neuston Net will be deployed many times over the course of the cruise.

Personal Log

Despite a bit of seasickness, I am having a wonderful time! Everyone on board is very welcoming and happy to answer my questions. Everyone is so busy! It seems like they have all been working nonstop since we arrived on board yesterday.

Answers to your questions

First, let me just say that these are great questions! Good job, Green Acres. Here are some answers, below.

1) How do the currents make a difference in the water temp? The currents play a major role in water temperature. In the Northern Hemisphere, currents on the east coast of a continent bring water up from the equator. For example, the Gulf Stream (which is a very important current down here in Florida) brings warm water from the tropics up the east coast of the United States. This not only keeps the water temperature warm, but it also affects the air temperature as well.

2) How does the current affect the different algae populations? Currents regulate the flow of nutrients (which phytoplankton needs to survive). Strong currents can also create turbidity, which means that it stirs up the water and makes it harder for light to penetrate the water column. As you know, phytoplankton rely on sunlight to grow, so if less light is available, the phytoplankton will suffer. I’m told by Sharein (one of the phytoplankton researchers) that algae are hearty creatures. This means that as long as the turbid conditions are temporary, algae should be able to thrive.

August 17, 2002March 18, 2021

Diane Stanitski: Day 7, August 17, 2002

NOAA Teacher at Sea

Diane Stanitski

Aboard NOAA Ship Ka’imimoana

August 16-30, 2002

Day 7: Saturday, August 17, 2002
Time: 0700 military time (based on a 24-hour time schedule)

Latitude: 21°14.715’North (N) Cruising just south of the Big Island of Hawaii visible this morning from the port (left) side of the ship when facing forward
Longitude: 157°57.378’West (W)

Weather Observations taken from the bow of the ship with Shippensburg University’s hand-held Kestrel 3000 instrument:

Air Temperature: 27°C (80.6°F)
Average Wind Speed: 6.3 knots (7.3 mph)
Cloud Cover: 8/10 with mostly altocumulus (middle level, puffy) and cirrocumulus (high level, puffy) clouds
Precipitation in previous 24 hours: 0 cm (0 inches)
Relative Humidity: 89%
Dew Point Temperature: 24.8°C (76.6°F) Relatively calm seas; beautiful sunrise; Porpoises spotted on the port (left) side of the ship

Quote written on the Plan of the Day (POD) posted outside the Main Mess (meal) area: “All excellent things are as difficult as they are rare.”
– Benedict Spinoza

After a restful night’s sleep on my upper bunk, I awoke ready for a new day! It struck me as I was lulling into a peaceful sleep that my mattress felt just like a waterbed. I thought that I was rolling around on a bowl of jello, a neat feeling which made me relax. I am fortunate that I haven’t experienced any seasickness yet. A few others haven’t been so lucky. Michelle, our fearless Medical Officer on board, has distributed medication for seasickness to those needing it. It is recommended that you breathe in fresh air and watch the horizon for a while if ever you feel queasy.

After touring the outer decks of the ship watching the sun rise above the morning clouds on the horizon, I stopped to speak with crew member Roger Stone who said that every day is slightly different because the sky is always changing. He recalled seeing a white rainbow at night under a full moon. I had never heard of this so I’m intrigued about what would cause such a remarkable feature.

Breakfast was interesting because I spoke with Rachel, a Cadet, and Steve, our Field Operations Officer (FOO) who received a degree in Meteorology at the University of Nebraska. We discussed Steve’s research and he said that I could come up to the bridge to take weather observations anytime. Yahoo! For some reason beyond me, weather obs are not everyone’s favorite activity of the day. Rachel taught me the difference between a pitching and rolling boat. She said that a pitching boat rocks front to back (up and down), while a rolling boat rocks side to side. She is currently taking a course requiring that she write a complete report of all of her activities while on board. I hope to learn many things from her, including celestial navigation — how to find your way using the stars. Can’t wait!

I learned from Steve that the reason it was a bit rocky in the ship last night was due to our travels through currents emerging from between the Hawaiian Islands. The currents disturbed the forward motion of the boat. Unknown to me, currents are named for the direction toward which they flow, unlike winds, which are named for the direction from which they blow. So, if ocean currents and winds are moving in the same direction, they have opposite directional names – very interesting!

I spent part of the day organizing my thoughts regarding my upcoming lesson plans. There are so many exciting ideas generated each day by the scientists as we talk. I will definitely interview the scientists on the ship about their current research as well as use the opportunity to describe the many mechanical and electronic sensors on board to everyone watching the webcasts. Please let me know what you would like to know more about and I’ll try to include it in a future webcast.

John pointed out flying fish on the port side of the boat today. They are quite small and it is believed that they fly to flee from whatever is gaining on them. They don’t have great ability to determine direction and they stay in the air for just a few seconds before splashing into the water again.

Our location and the weather observations at 1300 today were:
Latitude: 18°37.8’N
Longitude: 155°23.7’W
Visibility: 12 nautical miles (nm) which is about the greatest distance you can see due to the curvature of the earth
Wind direction: 060 (on a 0-360° scale) which means ENE
Wind speed: 19 kts
Sea wave height: 5-7′
Swell wave height: 6-8′
Sea Water Temperature: 26.6°C
Sea level pressure: 1015.0 mb
Dry bulb temperature: 26.2°C
Wet bulb temperature: 23.5°C

Sarah and Rachel gave me a tour of the ship’s bridge this afternoon. They discussed every aspect of their job and it was fascinating! They have radar on the ship to detect nearby ships and severe weather. On the front panel of the bridge there is an automatic pilot system for the ship. There are also throttles for the main engines, which allow us to travel at approximately 10-12 kts under ideal conditions. The bow thruster controls movement of the front of the ship from left to right. They described radio communication procedures with other ships, explained who has right of way when two ships are merging, and provided details about the nautical charts used during each journey. I made the mistake of calling nautical charts “maps” and was politely corrected. I will place this new term in my memory bank for future reference. I also was privy to a chart showing our upcoming transit line with waypoints approximately every 200 miles. The ship remains in a straight path until a certain point where a slight change of direction is made, otherwise, the bearing would constantly change as the ship’s path slowly curved.

After a workout and excellent meal of chicken stirfry, cauliflower, rice and pecan pie prepared by Helen and Doretha, I met with John who informed me that there would be a deployment of a test buoy tomorrow around 0900 and that he would like to videotape me on the buoy before it’s sent out to sea to explain the instrumentation on the mast. Earlier today I met with Dave and Paul, our Chief Scientists on board, and they explained the entire array of sensors and the purpose behind the buoy. It will be deployed and removed during this trip with data collected every few seconds and stored in a datalogger on the mast. During the return voyage of the KA to Honolulu in late September the buoy will be removed from the water and the data analyzed immediately following the trip. A compass comparison test and a buoy motion monitor test will be conducted. A specially engineered tube containing 3 different compasses and an accelerometer will enable the pitch, roll, and yaw of the buoy to be determined. As of yet, I believe that these movements on the buoy are unknown.

Today’s question: What is the pitch, roll, and yaw of a ship? Be the first to answer and I’ll acknowledge your response in my next log. I’ll write again tomorrow after a peaceful night under the millions of visible stars above.

Peace to all and to all a good night,
Diane