Tag: Alaska

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Nick Lee: Signing Off, July 21, 2024

NOAA Teacher at Sea
Nick Lee
Aboard NOAA Ship Oscar Dyson
June 29 – July 20, 2024

Mission: Pollock Acoustic-Trawl Survey

Geographic Area of Cruise: Eastern Bering Sea

Date: July 21, 2024

Science and Technology Log:

When I applied to the Teacher at Sea program, I was hoping to use my experience on one of NOAA’s cruises to enhance my AP Environmental Science class. Now, having just completed my time aboard NOAA Ship Oscar Dyson, I’m looking forward to incorporating pollock and fisheries research into my existing curriculum. The scientists’ research involved concepts that are already a key part of the AP Environmental Science curriculum, like biodiversity, sustainable fishing, and ocean currents. I’m excited to engage my students this year with more real life examples and photos from the cruise!

View of mountains from the bridge. The water is calm, and the snow-capped mountains are partially obscured by dramatic gray clouds.
View from the bridge on the last day of the cruise.

I wasn’t expecting to see as many applications of computer science on the cruise – however, I was surprised to learn how much of the scientists’ job on the ship involves coding and statistical analysis. At any given time, it seemed like at least one member of the science team was coding in Python or R, creating new programs and data visualizations that would help make their research more efficient and effective. We relied on many different computer applications to collect both acoustic and trawl data, almost all of which had been coded by the scientists and their colleagues.

MACE MasterApp, developed by scientists to collect and analyze data. This is a screenshot that shows a grid of icons labeled with program names such as "CLAMS QC," "Species Finder," "Transect Events," "Depth Comparison," and "Pies."
MACE MasterApp, the suite of apps the scientists use to collect and analyze data.

Some of these programs didn’t even exist just a few months ago, but they were created when someone on the team recognized an area for improvement. This represents a broader mindset of adaptability and collaboration I noticed among scientists. On the ship, plans constantly changed in response to weather, delays, and equipment malfunctions. While these could be frustrating, the scientists always looked for ways to still complete their research, troubleshooting with each other and with the other ship departments.

The science team on my cruise. Nine people pose for a group photo along a deck railing. Beyond them, we see calm ocean waters, green hillsides, and snow-capped mountains.
The science team on my cruise. From left to right: Mike Levine, Robert Levine, Dave McGowan, Abigail McCarthy, Taina Honkalehto, Moses Lurbur, Sarah Stienessen, Matthew Phillips, Nick Lee (Photo Credit: Emily Resendez).

I also learned how the scientists had been adaptable in their own careers. Most of the scientists I had worked with had not intended to study pollock when they were younger, and some had not even planned on studying marine science. However, when interesting opportunities presented themselves, they took advantage, even when this meant learning about a new type of research or traveling to a new location. Having different academic backgrounds meant the scientists had different perspectives, and each was able to contribute their own ideas on how to improve the group’s research. On this particular cruise, scientists were testing out cameras and studying pollock behavior at night in the hopes of improving their data collection methods for future surveys.

Personal Log:

I just arrived back in Boston after a few long travel days – I took a small boat from the ship to Dutch Harbor, and then I flew to Anchorage, then Seattle, and then finally Boston.

Small boat being lowered from the ship.
Sign warning of eagles. It's a wooden sign resting on the ground in front of a fence, reading "DANGER NESTING EAGLES," with a silhouette of a person with their arms in the air to shield their head from an attacking eagle. Nick does his best to reenact the pose, but there are no live eagles in sight.
From left to right: Small boat being lowered from the ship and an eagle warning sign in Dutch Harbor (Photo Credit: Abigail McCarthy).

I’m still processing my experience as a Teacher at Sea, but overwhelmingly I feel lucky to have spent three weeks aboard NOAA Ship Oscar Dyson and grateful to all of the people I met along the way.

The crew of the ship were all kind and welcoming, and I was able to learn about the other departments on board. I was able to tour the engineering department, and I learned how the ship makes its own freshwater by evaporating seawater. I shadowed the survey technicians as they deployed CTDs (conductivity, temperature, and depth sensor), and I touched water samples they had captured from the bottom of the ocean. During one trawl, I joined the deck crew, and I was able to witness how they safely manage nets containing thousands of pounds of pollock. Finally, I was able to learn about marine navigation from the NOAA Corps Officers, and I was even allowed to (briefly) drive the boat!

Engineering control room.
Nick streaming the net with the deck crew. He wears a heavy reflective coat, gloves, and a hard hat.
Learning to drive the ship. Nick, wearing a blue sweatshirt, stands at the helm and looks ahead. Emily stands nearby, arms crossed, looking in the same direction.
From left to right: Engineering control room, streaming the net with the deck crew (Photo Credit: Mike Levine), and learning to drive from NOAA Corps Officer Emily Resendez (Photo Credit: Savi Morales).

I want to thank all of the crew and officers of NOAA Ship Oscar Dyson for making the past three weeks such a meaningful experience, and I want to thank the science team for letting me contribute to their research and answering all of my questions (special thanks to Robert Levine for editing these blog posts)! Finally, I want to thank Emily Susko and the Teacher at Sea Program for supporting me throughout this entire process.

Did you know?

Applications for next season’s Teacher at Sea Program open in November – more info can be found here!

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Nick Lee: The Data, July 15, 2024

NOAA Teacher at Sea
Nick Lee
Aboard NOAA Ship Oscar Dyson
June 29 – July 20, 2024

Mission: Pollock Acoustic-Trawl Survey

Geographic Area of Cruise: Eastern Bering Sea

Date: July 15, 2024

Weather Data from the Bridge:

Latitude: 59° 51.9 N

Longitude: 173° 53.5 W

Wind Speed: 11 knots

Air Temperature: 6.1° Celsius (42.9° Fahrenheit)

Science and Technology Log:

On my cruise, scientists take acoustic measurements along the length of each transect. To ensure that they are accurately estimating the abundance of pollock, they take steps to separate out any backscatter that they believe didn’t come from pollock.

Scientists then apply algorithms to the data in order to estimate pollock abundance over the entire survey area. First, they break up the transect into 0.5 nautical mile (NM) sections and record the average backscatter for that section. Specifically, scientists are interested in the areal density – the amount of backscatter per square nautical mile (NM2).

This data can be challenging to interpret, so one way the scientists represent it visually is with a stick plot over the survey area:

Stick plot showing acoustic backscatter from the 2022 pollock survey. This is a simple map of the Bering Sea, where the land of Alaska appears in gray and the water is white with some bathymetric lines. The transect lines run straight, at a slight angle on this rotated map, across the waters. Yellow bars of different sizes stick up off the transect lines at an angle.
Acoustic backscatter from the 2022 pollock survey.

In this graphic, the transect lines are shown in black, and the density of acoustic backscatter for each 0.5 NM section is represented with a yellow stick. The longer the stick, the greater the density of backscatter at that location.

Scientists then use this data to perform calculations on the entire survey area, including the space in between transects. For each 0.5 NM section of transect, the acoustic density is extrapolated halfway to the next transect on either side.

Diagram showing transect lines, and how acoustic density is applied across the survey area. Three gray vertical lines, evenly spaced, are each labeled "transect line;" dotted lines mark the distance halfway between each transect line. A smaller portion of the middle transect line is colored red instead of gray. It's labeled with a parallel double-sided arrow marking out "0.5 nautical mile." A red box the height of that red section stretches as far to the left and right as the next dotted halfway line; one side is labeled "half distance to next transect."
In this diagram, the red line represents a 0.5 NM section of transect for which acoustic density is calculated. This acoustic density is then applied to the entire pink rectangle, which extends halfway to the next to the transect on either side.

By doing this process for every 0.5 NM section of transect studied, scientists are able to calculate values of acoustic density for the entire survey area.

Map of current survey area with transect lines and boxes showing the area over which transect data is extrapolated.
Map of current survey area and transect lines (black), with boxes (purple) indicating the area over which data from each transect is extrapolated.

Getting from acoustic density to pollock abundance takes another set of calculations, this time making use of trawl data. The pollock caught in each trawl can vary drastically in terms of size – some trawls are mostly juveniles, some trawls are mostly adults, and some are an even mix of both. For a given location, scientists use data from the nearest geographic trawl to estimate the distribution of fish in that area.

Distribution of pollock centered around 20-30 cm. This is a bar chart. The x-axis displays length in centimeters (0 to 80 cm) and the y-axis displays proportion of the catch (0 to 0.125). The majority of the bars are black, but a minor portion are colored partially red, indicating proportions of identified male pollock, or blue, indicating proportions of identified of female pollock.
In some trawls, the most fish were within 20-30 cm in length (above) while in others, most fish were over 40 cm in length (below).
Distribution of pollock centered around 40-50 cm. This is a bar chart. The x-axis displays length in centimeters (0 to 80 cm) and the y-axis displays proportion of the catch (0 to 0.125). The majority of the bars are black, but a minor portion are colored partially red, indicating proportions of identified male pollock, or blue, indicating proportions of identified of female pollock.

Having trawl data is necessary to convert the acoustic data into fish abundance because small and large pollock do not reflect backscatter equally. Scientists have studied this, and they have created a relationship for the different backscatter reflected by different length pollock. Using the distribution of pollock in the nearest trawl, scientists are able to proportionally allocate the observed backscatter to pollock of different lengths.

Graph showing that as pollock length increases, acoustic backscatter also increases. The x-axis shows pollock length in centimeters (0 to 80) and the y-axis shows acoustic size in "(TS, dB re 1 m2)", ranging from -50 to -30. A blue line curves gently from the lower right corner ("small fish, weak backscatter") to the upper right corner ("large fish, strong backscatter.")
As pollock length increases, backscatter also increases. 
(Equation from Lauffenburger et al., 2023. Mining previous acoustic surveys to improve walleye pollock (Gadus chalcogrammus) target strength estimates, ICES Journal of Marine Science, Volume 80, Issue 6, August 2023, Pages 1683–1696, https://doi.org/10.1093/icesjms/fsad094)

As an example, let’s simplify the two locations sampled in the graphs above. Suppose the first location had only 20 cm pollock, the second had only 40 cm pollock, and equal backscatter was observed at both sites. Scientists know that, all else being equal, 20 cm pollock produce less backscatter than 40 cm pollock. This means that in order to reflect the same backscatter, there must be a greater number of 20 cm pollock than 40 cm pollock.

By repeating a similar process for each geographic location, scientists are able to estimate the number of pollock in the entire survey area!

Personal Log

The sailing and many of the operations of NOAA Ship Oscar Dyson are done by NOAA Corps officers. I hadn’t heard of the NOAA Corps before sailing, but I’ve since learned that they play an important role in facilitating NOAA research.

To learn more about the experience of NOAA Corps officers, I interviewed Ensign Savi Morales.

Ensign Savi Morales working with John Swenson, a member of the deck crew. Engisn Morales wears the blue every day uniform of the NOAA Corps and stands at a bank of navigational computers on the bridge. Both men gaze down at a display screen.
Ensign Savi Morales (left) on the bridge collaborating with John Swenson, a member of the deck crew.

Why did you decide to become a NOAA Corps officer?

I’ve always wanted to support the protection of the environment and mitigating climate change. After college, I was trying to figure out where I would contribute the most. I really loved being out on the water, and I had sailed plenty but I wanted to find a way to combine my interests in an environment I contribute the most. The NOAA Corps felt like it was a combination of those things.

I also loved the idea of working with the crew, engineering department, and science. I really enjoy that mixture of groups we have aboard Dyson, which makes every trip’s dynamic different. There’s also a lot of hands-on experience on the bridge deck making our 12 days packed with projects I work on. The NOAA Corps embraces a diverse skill set in order to think and act like a Swiss army knife and be a jack of all trades.

What are your responsibilities on board the ship?

My responsibilities are two 4-hour bridge watches as a Junior Officer of the Deck as I work towards becoming a fully qualified Officer of the Deck. In between my watches I work on tasks related to my responsibilities as the Dyson’s damage control officer, assistant navigation officer, and assistant public affairs officer. I track the sea service hours for our augmenting and personal crew, which they can use to upgrade their license. I maintain flags, and I do monthly safety rounds, inspecting fire extinguishers and fire stations. 

What do you enjoy the most about your work?

I enjoy meeting the characters that come to the Dyson, definitely an eclectic but fun group. I also enjoy how much they’ve thrown me into the mix and had me figure things out. It’s a little bit of a trial by fire, but I learn really quick and I’d rather learn by doing.

What part of your job with NOAA did you least expect to be doing?

Checking fire extinguishers, there’s about 100 on board and they all need to be checked monthly. It takes about 3-4 hours.

Here in the Bering Sea you hear about the big, massive waves, but it’s not always like that. The Aleutian Islands are gorgeous with lots of wildlife. I don’t think I’ve seen this many bald eagles, orcas, or puffins in my entire life. They always brighten my day.

What advice do you have for a young person interested in a career in the NOAA Corps?

NOAA Corps requires you to have a four-year college degree in order to apply. Other than that, I’d say find opportunities to go out on the water. There’s high school scholarships, there’s college scholarships. You can also volunteer if you have time. I volunteered at the UC Davis Bodega marine lab. I visited once a week just to hang out with the scientists, with the crew to see if this is what I liked. Be curious and experience things for yourself!

Did you know?

NOAA Corps is one of the country’s eight uniformed services, and its officers operate NOAA ships and aircraft around the country. After completing basic training at the US Coast Guard Academy, NOAA officers assist in fisheries research, seafloor mapping, monitoring atmospheric conditions, and may respond to natural disasters and extreme weather. Learn more at the NOAA Corps website here!

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Nick Lee: Finding Fish, July 6, 2024

NOAA Teacher at Sea
Nick Lee
Aboard NOAA Ship Oscar Dyson
June 29 – July 20, 2024

Mission: Pollock Acoustic-Trawl Survey

Geographic Area of Cruise: Eastern Bering Sea

Date: July 6, 2024

Weather Data from the Bridge:

Latitude: 61° 15.0 N

Longitude: 174° 56.8 W

Wind Speed: 13 knots

Air Temperature: 5.3° Celsius (41.5° F)

Science and Technology Log:

On NOAA Ship Oscar Dyson, the science party’s mission is to understand the population of walleye pollock in the Eastern Bering Sea. To collect data, scientists rely on two main tools: acoustics and targeted trawling. Before any trawling can happen, scientists must first locate fish using acoustics, so I’ll be focusing on acoustics in this blog post – stay tuned for a post on trawling next time!

Scientists use two kinds of acoustics: active and passive. Many of my students are familiar with how bats use echolocation to navigate in the dark – active acoustics relies on the same principle. First, the echosounder on the ship emits a pulse of sound, or ping. This sound travels through the water and bounces off of objects that have different densities than water (such as fish, krill, or the ocean floor). The echosounder then “listens” for and records these echoes, also known as backscatter. Passive acoustics work similarly, except the echo sounder only listens for sound and doesn’t emit any itself.

illustration of a pulse of sound, depicted as a triangle, emanating from the bottom of a ship at the surface of the ocean. the triangle encompasses some of the sea creatures swimming by (depicted as simple white silhouettes) and ends at the ocean bottom.
The echosounder emits a pulse of sound, which gets reflected by objects of different densities, like pollock. Image Credit: Wieczorek, Schadeberg, Reid (2021) “How do Scientists Use Sound to Count Fish in The Deep Sea?” Frontiers for Young Minds. https://kids.frontiersin.org/articles/10.3389/frym.2021.598169

The greater the distance between the echo sounder and the object reflecting the pulse, the greater the amount of time between when the signal was emitted and backscatter. Based on this time, echosounder can determine the depth of the object producing the backscatter. This information is represented visually in an echogram:

Screenshot of an echogram. Backscatter is depicted as colored dots on a grid. in this case, the dots are densest and darkest at the shallowest depths (the ship bottom) and the deepest depths (the hard ocean botttom)
Screenshot of an echogram. The space between vertical grid lines represents 100 pings, and the space between horizontal grid lines represents 10 meters of depth.

The echogram shows depth on the y-axis and time on the x-axis. The intensity of backscatter is color-coded, where more intense backscatter is represented with red and brown, and less intense backscatter is represented with blue and green. The vertical grid lines represent all the backscatter from one ping, and the space between lines represent 100 pings.

On the cruise, pings are typically emitted at a rate of 1 Hz, or once every second. With every new ping, the echo sounder adds data to the right end of the echogram. This means that the horizontal grid lines represent the backscatter at one depth over time (or distance, if the ship is traveling at a constant speed).

At least one scientist monitors the backscatter throughout the duration of the transect. During the first day, the echogram was blank except for some lower-intensity backscatter near the surface and high-intensity reflection from the ocean floor. Because the mission of this cruise is to survey pollock, which tend to live at greater depths, we don’t pay much attention to the backscatter near the surface which is comprised of smaller organisms like krill. However, when scientists notice backscatter consistent with scattering from pollock, they may trawl to collect a sample for more detailed biological information.

Screenshot of two echograms showing low-intensity backscatter and high-intensity backscatter.
Echograms from two different locations showing low-intensity backscatter (left) and high-intensity backscatter (right). When the backscatter looks as it does on the right, the science team may decide to fish in that area.

As we traveled along the first transect line, there was very little backscatter that the science team thought represented pollock. Our CTD (conductivity, temperature, depth) measurements also showed that the water temperature was cold, right around freezing. This may suggest that we were traveling through the Bering Sea cold pool, a mass of cold water that forms from melting ice. This water tends to be too cold for pollock and other fishes, however, other animals, such as snow crabs, can still survive the lower temperatures. Fish like cod prey on snow crab, so the cold pool offers these crab an important refuge from predators. Read more about the importance of the cold pool for crab here!

GIF showing historical bottom temperatures in the Bering Sea from 1983 to 2018. The years 2015, 2016, and 2018 are notably warm.
Historical bottom temperature showing cold pool in blue / purple (Image Credit: NOAA Fisheries)

Personal Log:

The start of the cruise has been busy learning new faces, maritime practices, and scientific terms. However, in the past few days, with the help of meclizine (seasickness medication), I’ve begun to feel more settled and like I have some sense of routine.

When I’m on shift, I bounce around between a few different places. The science team tends to be in the acoustics lab, where we monitor backscatter and make decisions on when to fish.

Photo of the acoustics lab. Computers and many computer screens mounted on the wall above a long desk.
Acoustics lab, also called “the cave” for its lack of windows.

Once the scientists decide to fish, we first go up to the bridge, where NOAA officers control the direction and speed of the ship. The bridge has windows on all sides, so we’re able to make sure there are no marine mammals before putting the net in the water.

From the bridge, you can also see the trawl deck, where the deck crew works in collaboration with NOAA officers to put the net in the water. Once the fish are caught and hauled back to the ship, the science team processes the catch in the fish lab.

Photo of the bridge. Navigation computers surrounded by windows.
Photo of the trawl deck. Unspooled trawl net visible in A-frame.
The bridge and its view of the trawl deck.

When we’re not working, we’ll grab food from the galley / mess deck. The stewards on the ship serve three meals a day, but since I’m on the night shift, I often heat up leftovers or take advantage of the wide selection of snacks they leave out. There’s also a lounge, two gyms, and places to do laundry while at sea!

Photo of the galley, the ship's cafeteria. Tables and chairs, a refrigerator. Chair legs are capped with tennis balls to reduce sliding.
The galley, where food is available 24 hours a day!

Did you know?

NOAA Ship Oscar Dyson  has six onboard laboratories including a wet lab, dry lab, electronics lab, bio lab, acoustics lab, and hydrographics lab. Read more about the ship here!

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Nick Lee: First Days at Sea, July 2, 2024

NOAA Teacher at Sea

Nick Lee

Aboard NOAA Ship Oscar Dyson

June 29 – July 20, 2024

Mission: Pollock Acoustic-Trawl Survey

Geographic Area of Cruise: Eastern Bering Sea

Date: July 2, 2024

Weather Data from the Bridge:

Latitude: 59° 54.8 N
Longitude: 171° 54.9 W
Wind Speed: 14 knots
Air Temperature: 5.0° Celsius (41° F)

Science and Technology Log:

We’ve been sailing for just under two days, and I’ve already had an opportunity to witness lots of science aboard NOAA Ship Oscar Dyson! 

We spent the first day transiting to the start of the survey – I am part of Leg 2 for this cruise, and so we are picking up where Leg 1 left off. Since we won’t be able to find every pollock in the Bering Sea, we will need to rely on a representative sample, and then our data will be used to estimate the total stock.

The map below shows the intended path of our cruise, and the vertical lines represent transects, or lines along which we will collect data, spaced 40 nautical miles (or 74 km) apart so that we can cover the entire region with the time we have. Since we just recently arrived at the start of our survey, I’m still learning about the different data the science team will be collecting – more on that in a future blog post!

nautical chart of the Bering Sea, showing the land of Alaska to the east and a portion of Russia in the northwest. The cruise trajectory is overlaid in bold blue or red lines, with north-south transects connected by shorter westward connections. The blue transects start in Dutch Harbor and head west; the red transects are farther west
Map of the survey with the portion that I’ll be participating in shown in red, and the portion that has already been completed in blue.

On our way to our survey site, I was able to launch a drifter buoy through NOAA’s Adopt-a-Drifter Program. Unlike some other buoys, a drifter buoy is not fixed to the ocean floor. Instead, they float and “drift” with the ocean currents. Importantly, drifters are equipped with some sort of drogue – an underwater anchor. This way, the surface float (and the drogue) will move with ocean currents, but won’t be influenced as much by wind.

illustrated diagram of a drifter buoy. a white ball floats at the water line; this is labeled "Surface float - designed for moving on the surface with currents." The float has an Antenna, labeled: "the drifters transmit the data they collect as well as their position via satellite." Data is depicted as a gray triangle extending up from the antenna to a satellite in the sky, which is communicating with a satellite dish on land. Beneath the float, down into the water, extends a black cable, thicker toward the float. It's labeled: "Sensors: Sea Surface Temperature sensor and various measuring systems." The cable connects to what appears to be gray cylindrical tube, waving in the water labeled "Drogue: The buoys have some form of subsurface drogue or sea anchor."
Drifter Buoy diagram (Image Credit: NOAA Adopt a Drifter Program)

Deploying a drifter is as simple as dropping it into the ocean! I was able to deploy our first drifter last night off the stern (back of the ship). Our drifter was wrapped in biodegradable packaging for a safe deployment, but once in the water it should have opened up and extended to its full length.

a repeating video clip of Nick starting to toss the drifter buoy over the rail of NOAA Ship Oscar Dyson. he is wearing a helmet and a life vest, and looking away from the camera.
Deploying an ocean drifter.

Once deployed, the drifter transmits its location via satellite, and scientists are able to use this data to better understand ocean currents. You can track my drifter’s trajectory here!

In addition to a GPS that tracks location, drifters are often equipped with sensors for temperature, pressure, salinity, and more. Below is the path my drifter took in its first day after deployment, and the sea temperatures it encountered.

a map of a small section of the ocean between 191.2 to 192.0 degrees W and 55.4 to 56.2 degrees N. A series of colored squares form a small spiral in the middle; the squares range in color from orange to purple. Beneath the map there's a key explaining that the colors indicate temperature, ranging from purple (6 degrees Celsius) to red (7 degrees Celsius.)
Drifter trajectory and sea surface temperature.

I also was able to observe the deployment of a CTD (conductivity, temperature, and depth) sensor. CTD measure some of the same properties as drifters, but CTDs are lowered down into the water and then raised back into the boat. This means that CTDs only collect data at one geographic location at a time, however, they collect data throughout the entire water column, from the surface down to the ocean floor (~80 meters at our last deployment). CTDs can also collect water samples at different depths, allowing scientists to study them further. NOAA has a great resource on CTDs here!

view of the conductivity, temperature, and depth probe (in the center of a cylindrical metal apparatus) suspended from a cable just beyond the railing of the ship; it is about 10 feet above the ocean's surface at this point. in the distance, the sky is gray and cloudy, and the ocean is gray and calm.
CTD being lowered to collect data.

Personal Log:

When I applied to NOAA’s Teacher at Sea Program, I was told that one thing that was required of all its participants was flexibility. This is especially true for cruises leaving from Dutch Harbor, where bad weather and flight cancellations are common. On this leg, a series of travel delays meant that we left port a day later than expected. However, this meant that I was able to spend some time exploring Dutch Harbor!

Dutch Harbor is one of the most remote and beautiful places I’ve ever visited. During my wanderings around the town, I spotted whales, a fox, and plenty of bald eagles. Alaska’s military history is also apparent in the hills surrounding Dutch Harbor, which are full of World War II bunkers.

view of calm blue ocean waters from a green hillside; in the distance, two ships are visible
view under the archway of a bunker - there's sand underneath and open vegetation beyond
a bald eagle perches on driftwood on the beach
Views from Dutch Harbor (left), inside a World War II bunker (center), and one of many bald eagles (right).

Since we left port, there’s been a lot to adjust to about living on a ship. The ship is a bit of a maze – lots of narrow hallways and hidden staircases. After making a lot of wrong turns, I’m starting to get a sense of the layout.

Work happens on the ship at all hours of the day – I’ve been assigned the night shift (4 pm – 4 am), so as a natural morning person, I’ve completely changed my sleep schedule! Because someone is always working, that also means that someone is always trying to sleep, so I’ve learned to be careful about not letting doors slam behind me.

view of a stateroom: two berths (bunk beds), a chair, a window with curtains, a hiking backpack and a bag.
My stateroom for the next three weeks.

This morning, we practiced our first set of safety drills. To simulate what would happen if we needed to abandon ship, everyone was required to don a survival suit (also called a “Gumby suit”). It was quite a process to put on the suit – luckily one of the other scientists, Mike, gave me some pointers ahead of time!

Nick poses, thumbs up, for a photo in the survival suit; it covers his mouth and nose
Gumby suit

I’m looking forward to learning more about life at sea over the next few weeks!

Did You Know?

NOAA Ship Oscar Dyson was named after an Alaskan fisherman and activist who worked to improve the industry for other Alaskans (https://www.omao.noaa.gov/marine-operations/ships/oscar-dyson )

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Germaine Thomas: Meet the Teacher at Sea on NOAA Ship Oscar Dyson, August 9, 2023

NOAA Teacher at Sea

Germaine Thomas (she/her)

Aboard NOAA Ship Oscar Dyson

August 7 – August 21, 2023

Mission: Acoustic Trawl Survey (Leg 3 of 3)
Geographic Area of Cruise: Pacific Ocean/ Gulf of Alaska
Date: Wednesday, August 9, 2023

Weather Data
Lat 58.16 N, Lon 148.97 W
Sky condition: Cloudy
Wind Speed: 2.88 knots
Wind Direction: 301.28°
Air Temp: 12.44 °C

Personal Log

School will soon be starting in Anchorage at Bettye Davis East High School. I will not be in school for the first three days because I am having fun on a teacher’s field trip. Good things come to those who apply for it. I applied and got accepted on this cruise before the pandemic, but life and safety concerns made my journey about three years longer. Finally, I am living the dream and out in the Gulf of Alaska surrounded by pure ocean, whales, seabirds and catching lots of fish.

selfie of Germaine on a kayak (too close to see the kayak, but we can see she's surrounded by water, with some forested shoreline beyond.) she wears a life jacket, sunglasses, baseball cap. A small white dog peers over her left shoulder.
Kayaking in Prince William Sound with Loki the dog. My family commercial fishes for Sockeye Salmon in Main Bay.

My name is Germaine Myerchin Thomas. I was born and raised in Ketchikan Alaska. I am the daughter of a fishermen and a teacher. I, myself, am a teacher, and I commercial fish in Prince William Sound. So far I have spent most of my summer fishing in the Eshamy district about 45 miles outside of Whittier. It has been a cold dark wet summer( the word “summer” is debatable). Recently, I jumped from Set Net fishing for Sockeye (Red) Salmon, in small open skiffs, to the fabulous NOAAS Oscar Dyson.

Just visualize the ice sculptures, swimming pool and yoga studio on the Lido Deck… nope! The NOAAS Oscar Dyson is a research vessel that you can find more about by clicking the link above. Currently there are 24 crew members and 8 scientists. The ship is outfitted to conduct an acoustic trawl survey, but there are other scientific projects going on during this leg of the cruise. It, also has great food and two gyms. The waves rolling under the hull of the boat make the feel of gravity extra strong while trying to do push ups.

Already I have discovered that working out in the ocean requires being very flexible and adaptable. Sometimes the weather or wildlife can delay setting out the trawl net. Last night the boat was surrounded by whales (Fin and Sei), marine birds (Fulmars, Shearwaters and Black footed Albatross) all enjoying the abundant fish that we wanted to catch in our trawl net. Naturally we just let the animals enjoy the abundance while the scientist patiently waited for their turn in another area.

When the cruise ends I will head back to Anchorage and teach high school, chemistry, oceanography, and marine biology. I am really looking forward to meeting my students for the first time. I hope that I might be able to Zoom into my classroom and share what I am doing while I am out here.