Sam Garson: Everybody’s Trawling for the Weekend, September 12, 2024

NOAA Teacher at Sea

Sam Garson

Aboard Henry B. Bigelow

September 6 – 25, 2024

Mission: Leg 1 of Fall Bottom Trawl Survey

Geographic Area of Cruise: Mid-Atlantic Coast

Date: September 13, 2024

Weather Data from the Bridge:

Latitude: 36.93°N
Longitude: 76.3°W
Wind Speed: E 15 G 21 mph
Air Temperature:
22°C (71°F)

Science and Technology Log

NOAA’s Fall Bottom Trawl Survey began in 1963 and holds the distinction of being the longest-running standardized fishery-independent scientific trawl survey in the world. Its primary goal was to monitor the abundance and distribution of fish species in the northwest Atlantic Ocean, particularly on the continental shelf stretching from Cape Hatteras, North Carolina, to the Gulf of Maine. However, over time, the survey’s role has evolved into something far greater.

With over 60 years of continuous data collection, this survey is not only an important resource for understanding fish population dynamics, but it also serves as a data source for marine research across the globe. The data gathered provides unparalleled insights into long-term trends in marine ecosystems, making it a cornerstone of NOAA’s fisheries management program. This consistency allows scientists to assess how various factors—such as fishing pressure, environmental changes, and oceanographic conditions—affect fish populations over time.

By maintaining strict protocols and procedures across the decades, NOAA ensures that the data collected remains comparable year after year. As a result, this long-running trawl survey is a powerful tool for detecting shifts in marine biodiversity, population fluctuations, and changes in habitat use among species. The findings from the survey inform not only U.S. fisheries policy but also global conservation efforts, positioning it as a keystone project for marine resource management. The enduring nature of the Fall Bottom Trawl Survey has provided a reference point for understanding the impact of climate change on marine ecosystems, as rising ocean temperatures and shifting currents are increasingly influencing species distribution.

view from the distances of the ship underway. it's a cloudy day, gray skies and water, and the image itself is a little cloudy - we can't make out the NOAA logo or ship number on the hull.
NOAA Ship Henry B. Bigelow. Photo Credit: Sam Garson
a diagram of NOAA Ship Henry B Bigelow showing the plankton net, trawl net, and sonar capabilities. title: State of the Art Research Vessel Henry B. Bigelow. box labels identify the following features: (1) Navy designed "quiet" hull does not disturb marine life. (2) Advanced 3-D sonar gives researchers a bigger picture of fish and their marine habitat. (3) Plankton net gives an accurate survey of fish food supply. (4) Fish net can help gauge abundance of fish stocks.
Illustration credit: James Warren / Cape Cod Times, Information source: NOAA

How Does a Trawl Work?

Members of the Bottom Trawl team work in 12 hour shifts, Midnight to Noon and Noon to Midnight. When it is your turn on watch you will wait for the ship to reach the next “station” or sampling site. Once there the survey team will deploy a CTD and possibly a “Bongo” plankton tow.

two crewmembers wearing hard hats, life vests, and gloves stand on the deck of the ship near a large piece of scientific equipment. the conductivity, temperature, and depth probe, along with one water sample bottle, is mounted inside a cylindrical metal frame attached to a cable.
Crewmembers ready to deploy the CTD.

Once on station, the ship will deploy and stream the trawling net for between 16 and 20 minutes at a specified depth. Far from a simple task, this operation of the net streaming behind the ship is monitored closely with technology and data. The watch lead has to work closely with the bridge to ensure that the trawl net is running through the water properly. Monitoring the opening, speed and depth throughout the dive. Once all of that is confirmed to be in good working order you’ll hear the call over the PA, “HAUL BACK!”

photo of a computer screen showing a plot. on the x-axis is time. the y-axis shows depth and "TE Height," and there are three plot lines.
Trawl net monitoring. Photo Credit: Sam Garson

Haul Back

Once the “haul back” call is given the deck crew springs into action to bring the net back on deck, while the science team moves into position in the sorting room. This process starts in the ready room, where everyone keeps their foul weather gear and gloves.

view of a collection of orange rain coats, orange overalls, and large rubber boots spilling out of a closet-type area on one side of a room
Ready Room. Photo Credit: Sam Garson

Once in their foul weather gear, the team will move to their positions along the first of three main conveyor belts. One member of the team will move out to the checker box where all of the trawl contents are first placed. From there the checker will feed the marine life into the first conveyor belt that brings all the specimens up to the main conveyor belt. Here the marine specimens are all sorted into buckets and bins by species, size and sex. The watch leader will tell the team what they are going to “run” that trawl, meaning which species do they leave on the belt to be deposited into bins at the very end. Depending on the goals, catch diversity or needs the watch leader could run everything from squid or crabs to sea robins.

view inside the wet lab. there are rows of stations, each comprised of a metal table with a measuring board, a drainage sink, a work surface, a computer monitor.
Cutting Station. Photo Credit: Sam Garson

Now that everything is sorted into buckets and bins the real data collection begins! The watch is broken into teams of two. A recorder and cutter work together to process every single marine sample for a variety of data products. These trawls are incredibly productive and have lots of scientists from institutions around the country sending in requests for samples and data. This is where the computer screens are so critical. As buckets of samples move down the last conveyor belt, the cutter scans them into the system and then is prompted by the computer to walk through any number of data collection procedures. The recorder enters them all into the computer, bags the samples, and processes the documentation needed. On this cruise we have been freezing samples, collecting otoliths (unfamiliar? check out this great NOAA resource), collecting stomachs and measuring and weighing hundreds of different species across all of our trawls.

Once that is complete we clean our stations and get ready for the next trawl. Sometimes this could be 30 minutes away, or even an hour, at times. It can be instantly after completing the last trawl. Working in 12 hour shifts, 24 hours a day means that the amount of data we are producing and cataloging is massive, but so is the job of sampling on the scale needed to help scientists answer questions about the ecology, populations, diversity and impacts of climate change along the Eastern Seaboard.

Personal Log

It’s been 10 years since I last sailed and I have been amazed at how quickly I’ve fallen back into the swing of life at sea. The night shift from 12:00 AM – 12:00 PM was a rough adjustment at first, but pretty quickly my body adapted and I settled into the routine.

It has been incredibly interesting to compare my previous time on an ROV based exploration vessel with the reality of a trawl based research mission. The E/V Nautilus was my home for 7 years and walking around the Bigelow definitely brings back some amazing memories, but it also has been a great reminder of how different things are across platforms. The ins and outs of life on Bigelow and the pace of the trawl are worlds different from the 24 hour ops of the ROV missions. I’ll write more on that later, but it has been a really cool comparison to make. It will be interesting to see how the rest of the cruise goes as we are only 3 days into our mission, and lots of cool fish still to come!

Did You Know?

Henry Bigelow was one of the key members of the scientific community who helped found Woods Hole Oceanographic Institute, here is an amazing photo of Henry Bigelow with WHOI’s mascot!

a scanned black and white photograph. A man, dressed in a 3 piece suit and white hat, stands on the deck of a ship - the shoreline is visible at the horizon. he braces himself, his left foot positioned back, because a goat standing it on its hind legs is pushing against his chest with its forelegs. the man holds something with both hands, up toward the goat's face - maybe food.
Henry Bigelow and Buck the WHOI Mascot (1904). Photo Credit: NEFSC NOAA

Patricia Kassis, June 10, 2008

NOAA Teacher at Sea
Patricia Kassis
Onboard Research Vessel Kilo Moana
May 23 – June 10, 2009

Mission: Woods Hole and Hawaii Ocean Time Series
Geographic Region: Hawaiian Islands
Date: June 10, 2008

Science Log

We have remained at the buoy site today. We continue to do the meteorological measurements from the bow (sea surface temperature and humidity), we did a single CTD cast just to test that the instruments were working right for the next cruise, and we’ve been monitoring the data from the new buoy and comparing them to data the ship is collecting.

The mooring data we’ve been watching especially closely is the wind direction, which was off before we replaced the anemometer yesterday. And it turns out… the wind direction is still off. The two anemometers still record a difference of about 30 degrees. Although it took a few hours to get the first readings, we were immediately skeptical that the fix had worked because the old “broken” anemometer seemed to be in good working condition when it was brought back on board. The trouble is directional (the instrument’s speed measurements are consistent), and it turns out that the compass in each anemometer is influenced by the magnetic field created by the bird wire. Why didn’t they think of this? Well, they did, but the bird wire was not supposed to be magnetic. It turns out that we can deflect a compass by bringing it close to some bird wire. This also means that the other anemometer is probably reading an erroneous direction too, as it is surrounded by bird wire also. So the big wigs are bustling around now trying to make an algorithm to correct the wind direction data. In short, we hope the wind direction readings are always deflected by some predictable amount, so we should be able to adjust the data before using it. Shipboard wind measurements will help calculate the errors.

By request, here’s a close-up of the meteorological instruments on top of the buoy.

met_closeup

From left to right, they are:
Temp and Humidity sensor (white cylinder with horizontal stripes)
Rain Gauge (white cylinder with opening at the top, black inside; also associated metal cylinder)
Anemometer (with propellers, in the back)
GPS unit for location data (orange)
GPS unit that transmits via Iridium connection (while cylinder)
Barometer for measuring atmospheric pressure (metal cylinder)
A light that flashes orange at night – in the back, here it is covered with black plastic
Four sunlight radiation detectors in the middle (two long-wave, two short-wave)
Second Barometer (metal cylinder)
Second anemometer
Iridium antenna (cylinder with larger diameter)
battery pack (metal cylinder)
second rain gauge
second temp/humidity sensor

The data that these instruments collect are available in nearly real time for the public to see. Right now, the website is still picking up info from the old buoy, which is sitting on deck and, therefore, not making sense. But if you check this WHOI website later on, you should be able to see graphs of barometric pressure (BPR), air temperature (ATMP), water temperature (STMP), wind speed (WSPD), wind direction (WDIR), relative humidity (RH) and so on. Each quantity is measured by two instruments, so each graph has two lines – hopefully they are close; often they are so close it looks like one curve. But let’s keep an eye on that WDIR – a good algorithm will place the two curves close together.

Personal Log
Tonight will be our last night at sea. We’ll leave the buoy area around sunset tonight and head toward Honolulu. We’ll enter the harbor around daybreak and spend the day unloading equipment.

Patricia Kassis, June 8, 2008

NOAA Teacher at Sea
Patricia Kassis
Onboard Research Vessel Kilo Moana
May 23 – June 10, 2009

Mission: Woods Hole and Hawaii Ocean Time Series
Geographic Region: Hawaiian Islands
Date: June 8, 2008

Buoy alongside the ship
Buoy alongside the ship

Science Log

These couple of days have been relatively calm science-wise, but the seas are the biggest we’ve seen. It’s not stormy or choppy, but big swells rock the ship with a low frequency, especially yesterday. Accordingly, the small boat mission to fix a wind instrument (anemometer, not flute) on the buoy was postponed until today, and it went pretty smoothly despite, in my opinion, pretty big swells. Here are a couple of shots of the mission. The first shows the launch. After the occupants pile in, the boat is lowered from a height of 15 or 20 feet. You can see the buoy (a speck just above the green arm of the crane), and the captain above – in a t-shirt and jeans.

The second photo shows Sean (only his legs are visible) climbing on the buoy while the boat circles. I don’t think these stills convey how the seas are moving, which I’d estimate as 7 foot high faces and wavelengths of about 300 feet. Even tough guy Sean quietly requested some food to help settle his stomach afterwards. The last CTD cast wrapped up yesterday.

We continue to collect more science data. We’re constantly monitoring data from the new buoy; a job powered mainly by computers and overseen by capable experts. Additionally, all along we’ve been doing some low-tech data collection. I’m actually surprised that this data is even taken, and I’m not sure of the extent to which these numbers influence science findings. Here is the psychrometer, a gadget with a fan (on the right, encased in metal) to rush air over two thermometers, one bare “dry” one, and a “wet” one with a thin wet sock covering its bulb (hidden by a metal sleeve). We record the two temperatures, and then use an equation or table to compute the relative humidity.

Here's a picture of some helpers like me "tagging" the lines - that is, steadying the rosette on its way back on board.
Here’s a picture of some helpers like me “tagging” the lines – that is, steadying the rosette on its way back on board.

The whole contraption is lowered into the upper ocean using a rope, brought back up without spilling (luckily, the geometry makes this easy), and the sea surface temperature is read off of the thermometer before the water is dumped out. This is pretty unsophisticated stuff, but it is the most reliable method we have for measuring the sea surface temperature. (CTD’s are too deep and satellites can be fooled by a slightly different temperature in a skin atop the surface.)

Here is the thermometer we use to measure sea surface temperature. It is a small PVC bucket with a fixed thermometer suspended in it.
Here is the thermometer we use to measure sea surface temperature. It is a small PVC bucket with a fixed thermometer suspended in it.

Personal Log

I am on watch from 7 to 11 in the morning, and again from 19 to 23 at night. So I’ve had a lot of free time in the middle of the day. I bug some scientists and technicians to show me the data they were playing with, but I also got laundry done and have enjoyed some ice water and a good book. I actually picked up a little sunburn – was my sunscreen too little, too late or too infrequent?

SST_bucket

Patricia Kassis, June 6, 2008

NOAA Teacher at Sea
Patricia Kassis
Onboard Research Vessel Kilo Moana
May 23 – June 10, 2009

Mission: Woods Hole and Hawaii Ocean Time Series
Geographic Region: Hawaiian Islands
Date: June 6, 2008

Downloading data from the CTDs
Downloading data from the CTDs

Science Log

Science efforts today seem to be split between removing things from the recovered buoy and collecting more data with CTD’s. Part of what we’re getting off of the buoy is that data stored in the CTD’s that hung beneath it. Here’s Jeff (with a corny look on his face) downloading this data. He’s got 6 CTD’s going at once, and the process takes hours.

Also coming off the buoy are the atmospheric instruments on top. Here’s a shot of Sean working on that while Jim moves cable from the winch that pulled it on board onto the spools where it is stored. My roommate Tenley is operating the winch.

The CTD casts have started back up (we took a break from that to recover the buoy), which means I’m on a work shift – about 4 hours on and 8 hours off. I start tonight at 7 pm. I’ve done 2 casts so far, and I’m already getting to be more helpful, successfully steadying the CTD rosette from the deck.

tenleyWinch

Personal Log

Buoy on deck
Buoy on deck

I got to do laundry yesterday. This was a real treat since I arrived at this cruise directly from another trip, already with a sack of dirty clothes. There are two washers and two dryers on the ship and about 35 people on board, so there’s a restriction on when someone can use the machines. For the science party, of which I’m a member, the laundry is available Friday, Saturday and Sunday. That means tomorrow will be my last chance before jetting off on another trip, so I’ll be visiting the laundry room again. We had filet mignon for supper last night and I’m not even kidding.
Hey Parker ‘Ohana, is anyone reading this? When people on the ship find out what I’m doing here, they keep asking what feedback I’m getting from my students and my school. I’m sad to report “none!” So if you’re reading this, and you’re a Parker person, drop me a comment or a line (mrskassis@hotmail.com) so I know I’m not just talking to myself (or typing to myself, I guess.) If you have any questions, or if there’s anything you want me to photograph, I’m happy to accommodate.

Patricia Kassis, June 5, 2008

NOAA Teacher at Sea
Patricia Kassis
Onboard Research Vessel Kilo Moana
May 23 – June 10, 2009

Glass balls
Glass balls

Mission: Woods Hole and Hawaii Ocean Time Series
Geographic Region: Hawaiian Islands
Date: June 5, 2008

Science Log

The old buoy came back on board today. First, an acoustic signal was sent to a device located just above the anchor, which released, severing the connection between the anchor and the 80 glass balls above. These glass balls (encased in yellow plastic) are buoyant, but they live deep underwater. They keep the bottom of the rope off of the sea floor and the anchor, and they aid in recovery. The balls come speeding up, but since they have such a long trip, it takes them 40 minutes or so. I guess sometimes balls get crushed on descent, and others on ascent, so the pile of recovered glass balls includes some that are destroyed. One is shown here. Then came miles of nylon and synthetic line, enough to refill those empty boxes, and then the instruments began coming aboard (CTDs and current meters). First came the deepest instruments, looking shiny and new. At slightly shallower depths, we began to see some biology – some nice clean mussel-ish thingies as big as your thumb.

Things growing on the buoy
Things growing on the buoy

Then the buoy itself came aboard. While it is floating, you can’t remove all the instruments below it or it becomes unstable, without that weight pulling it down. So before the last submerged instruments came up, the buoy came aboard. This was a rocking, dangerous, awkward event, with the buoy slamming against the ship. When I asked if this buoy recovery was typical, I was told, in the nautical style of curt understatements, that this was “not a good one”. The buoy itself was covered with barnacle-like things, crabs, slime and, on top, bird droppings. If you got sick in the zoo’s bird house, cleaning this baby is not a job for you. (Cleaning this baby was, by the way, a job for pretty much every science person on board, from chief scientists and technicians on down to lowly observers like me.)

After the buoy was on deck, we recovered the shallowest, and thereby most biologically covered instruments. These had critters and slime. The sticker on this one says “25 meters”. Can you read it? Can you find it? I was on watch until 4 am this morning, so I actually slept through the early stages of buoy recovery, specifically the glass balls ascending. I woke up for lunch (beef pot pie – the beef bearing significant resemblance to last night’s prime rib. I’m not complaining, leftover prime rib is a-okay with me!)

The area around the old buoy was fertile fishing ground, but the scientists require everyone to wait until everything is recovered before casting. This is to avoid tangling fishing lines around science tools. During the nearly daylong recovery operation, the fishermen aboard were salivating over the mahimahi and ahi they saw circling. Finally, they got two lines in and quickly caught two small ahi. Here’s Paul, who gets the award for catching the first.

He was a little embarrassed to strike a pose with a relatively small fish, so I promised him I’d throw this picture away once he catches a bigger one. As of press time, he’s had no such luck.

Buoy comes aboard
Buoy comes aboard

Barnacles!
Barnacles!

Shallow instruments have the most growth
Shallow instruments have the most growth

Catch of the day!
Catch of the day!