Tag: seabirds

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Donna Knutson, September 19, 2010

NOAA Teacher at Sea Donna Knutson
NOAA Ship Oscar Elton Sette
September 1 – September 29, 2010

Mission: Hawaiian Islands Cetacean and Ecosystem Assessment Survey
Geograpical Area: Hawaii
Date: September 29, 2010

Visitors of the Monument

Back in the boat trying to get a biopsy from pilotwhales.
Mission and Geographical Area:  

The Oscar Elton Sette is on a mission called HICEAS, which stands for Hawaiian Islands Cetacean and Ecosystem Assessment Survey.  This cruise will try to locate all marine mammals in the Exclusive Economic Zone called the “EEZ” of Hawaiian waters.  The expedition will cover the waters out to 200 nautical miles of the Hawaiian Islands.

Data such as conductivity, temperature, depth, and chlorophyll abundance will be collected and sea bird sittings will also be documented.
Science and Technology:
Latitude: 26○ 33.6’ N
Longitude: 177○ 05.5’ W  
Clouds:  3/8 Cu,Ac, Ci
Visibility:  10 N.M.
Wind:  12 Knots
Wave height:  4-6 ft.
Water Temperature: 27.8○ C
Air Temperature:  26.8○ C
Level Pressure:  1024.0 mb
Female Great Frigatebird is a large bird with a wingspan up to 86 in.
They do not walk or swim and are the most aerial of the seabirds.

The Northwest Hawaiian Islands became a Marine National Monument called Papahanaumokuakea Marine National Monument.  Papahanaumoku is a mother figure represented by the earth.  Wakea is a father figure represented by the sky. They are the honored and  highly recognized ancestors of Native Hawaiian people.  Together they resulted in the creation of the entire Hawaiian archipelageo and naming the Northwestern Hawaiian Islands after these names to strengthen Hawaii’s cultural foundation.

Layson ducks are only found on Laysan and Midway.
They were near extinction from hunting and invasive species, now they are protected and their numbers have increased to over 500.

Papahanaumokuakea is considered a sacred area. Native Hawaiians believe that life springs from this area and spirits come to rest there after death.  That means they also believe that they are descended from the same gods who birthed the Hawaiian Archipelago and it is therefore their responsibility to become stewards to care for the natural and cultural resources in Papahanaumokuakea.

Short-tailed Shearwaters often fly in flocks. These birds were on their migratory route.

The HICEAS cruise has track lines that cross into the National Monument, so while in the Monument, we must abide by the rules set forth to protect the natural and cultural resources within.

 This area is indeed rich in life as well as tradition.  Over ninety percent of the Monument’s area is deep sea.  Some depths are greater than three thousand feet. Hawaiian monk seals may travel more than one thousand feet down into the ocean to feed on gold and bamboo corals.  Some of the corals are over four thousand years old.  Scientists are just beginning to understand deep sea habitats such as that of sleeper sharks, hagfish and crabs.
Even though there is not much land within the monument, many animals make it their home.  Over fourteen million seabirds of twenty-two different species breed and nest in less than six square miles.  The reason these islands are so populated is because of the island’s isolation and conservation measures.
White tern on Midway. The oldest White terns on the island are 50years old!
The greatest threat of the Monument is climate change.  An increase in sea surface temperature is linked to disease and coral bleaching.   Rising sea levels cause less land for green sea turtles, monk seals and seabirds.
The HICEAS cruise has documented thirty-seven species of seabirds.  Not all of these birds live on the islands, many are migrating.  Within the “tubenosed” , Procellariformes  order, there are the Petrels and Shearwaters.  The Petrels include the Kermadec, Herald, Hawaiian, Juan Fernandez, White-necked, Back-winged, Bonin, Wilson’s Storm, Band-rumped Storm, Cook’s, and Bulwer’s.  The Shearwaters include the Christmas, Wedge-tailed, Buller’s, Sooty, Short-tailed, and Newell’s.
Bonin petrels are coming back to their burrows on Midway.
The burrows may be 9ft. long and 3 ft. underground.

From the order Pelicaniformes the Red-tailed and White-tailed Tropicbird have been recognized and also the Brown, Red-Footed, and Masked Bobby.   Great Frigatebirds, the largest of all within this order, have also been seen soaring high above the ocean.

A third order is the Charadriiformes, the shorebirds, terns and jaegers. The HICEAS track line is bringing us close (within three miles) to the shores of atolls and islands so therefore shore birds are seen as well.  The shore birds seen so far are the Bristle-thighed Curlew, Pacific Golden-Plover, Red Phalarope, Ruddy Turnstone, Bar-tailed Godwit, the Brown and Black Noddies, the White, Sooty, and Grey-backed Terns, the Pomarine, Parasitic, and Long-tailed Jaegers, and the South Polar Skua.
The HICEAS cruise will agree with the National Monument in proclaiming this area has an abundance of seabirds!
Personal Log:
The bottom view of a Wedge-tailed Shearwater.
Like most seabirds, they mate for life.

My roommate or “statemate” (on ships there are no bedrooms rather staterooms) is Dawn Breese, she is an avid Birder.  Scott Mills, also a Birder mentioned in Log #2, have been noticing a trend in their daily bird population densities.

As we headed northwest, they noted on September 17, 2010 when the Sette was at 28○ 24.7’ N and 178○ 21.1’ W, they saw their last Short-tailed Shearwater.  They did not see any Short-tailed Shearwaters after those coordinates and felt that it was odd considering the large amounts they had seen previously.  Near the International Dateline past Kure we headed back southeast once again and the Short-tailed Shearwaters reappeared at 27○ 6.28’ N and 178○ 27.9’W.  They concluded that they had passed twice through the Shearwater’s migratory route and seemed to find its NW edge.  On a single day alone, they estimated that there were over fourty thousand birds in that area!
White-tailed tropicbird likes to plunge dive for fish and squid.

When they mentioned the huge numbers of Short-tailed Shearwaters they saw, I decided to do some checking on them. I discovered the Short-tails are about forty centimeters long and have a wing span of 100 centimeters.  It is chocolate brown with a darker brown cap and collar.  It is often observed in large flocks and will dive fifty meters into the ocean for fish and squid.

Juan Carlos brought the Wedge-tail Shearwater down for Dawn to see.

The Short-tails breed on islands off southeastern Australia and migrate north to feed in the Bering Sea.  The Sette crossed their route flying back to the South Pacific!  It is a good thing they are “tubenosed” because they will not land until they have reached their destination.  The “tubenose”, (mentioned blog #2), will help the birds eliminate salt from their bodies.  Some short-tails on the breeding grounds will actually commute to the Antarctic to feed on fish along the ice.

The Wedge-tails tubenose is on the top of the beak.

On September 20, 2010 Juan Carlos knocks on our door after sunset to show Dawn a Wedge-tailed Shearwater, cousin of the Short-tailed Shearwater. The nocturnal animal got distracted by the ships’ light, and ended up on deck.  According to the Hawaii Audubon Society, Wedge-tail Shearwaters on O’ahu are often hit by cars because of the car’s lights at night.  O’ahu and Kaua’I both have rescue shelters for hurt birds from car accidents.

The Wedge-tail posing with Dawn and I.

Juan Carlos rescued the stunned bird, making sure it could not bite him with its sharp beak, and brought it down to show the bird observers.  I took close-ups of the bird because I wanted a picture of its tubenose.  Dawn showed me the unique features of the Wedge-tail.  It smelled fresh like a sea breeze.  We looked for the small ears behind the eyes but it’s feathers were so dense we couldn’t get a good look at it.

The bird had light brown feathers with a white belly, it was very soft and dainty looking.  It didn’t seem to mind people staring at it within a ship, but it probably just seemed content because Dawn knew the correct way to hold a bird.  After the Wedge-tail was checked out, Dawn took it up to the fantail (back) deck and released it.   The bird flew away unhurt into the night.
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Kathryn Lanouette, August 1, 2009

NOAA Teacher at Sea
Kathryn Lanouette
Onboard NOAA Ship Oscar Dyson
July 21-August 7, 2009 

Mission: Summer Pollock Survey
Geographical area of cruise: Bering Sea, Alaska
Date: August 1, 2009

This sonar-generated image shows walleye pollock close to the sea floor. The red line at the bottom of the image is the sea floor. The blue specks at the top of the image are jellyfish floating close to the water’s surface.
This sonar-generated image shows walleye pollock close to the sea floor. The red line at the bottom of the image is the sea floor. The blue specks at the top of the image are jellyfish floating close to the water’s surface.

Weather Data from the Ship’s Bridge 
Visibility: 10+ nautical miles
Wind direction: variable
Wind speed:  less than 5 knots, light
Sea wave height: 0 feet
Air temperature: 7.9˚C
Seawater temperature: 8.6˚C
Sea level pressure: 30.1 inches Hg
Cloud cover: 7/8, stratus

Science and Technology Log 

In addition to the Aleutian wing trawl (which I explained in Day 5 NOAA ship log) and Methot (which I explained in Day 8 NOAA ship log), scientists also use a net called an 83-112 for bottom trawls. The 83-112 net is strong enough to drag along the sea floor, enabling it to catch a lot of the animals that live in, on, or near the sea floor. This afternoon, we conducted the first bottom trawl of our cruise. Bottom trawls are usually conducted in two situations: if the walleye pollock are too close to the sea floor to use an Aleutian wing trawl or if the scientists want to sample a small amount of fish (because the 83-112’s net opening is smaller than the Aleutian wing trawl’s net). From the looks of the sonar-generated images, it appeared that most of the walleye pollock were swimming very close to the bottom so the scientists decided it would be best to use the 83-112 net.

Here I am holding one of the skates that was caught in the bottom trawl
Here I am holding one of the skates that was caught in the bottom trawl

Once the fish were spotted, we changed our course to get ready to trawl. Usually the trawl is made into the wind for stability and net control. Once the ship reached trawling speed, the lead fisherman was given the “OK” to shoot the doors. Slowly, the net was lowered to 186 meters below the surface, the sea depth where we happened to be. The water temperature down there was about 1˚C (compared to 7˚C on the sea’s surface).  I had heard from a previous Teacher At Sea that bottom trawls brought up a wide variety of animal species (compared to the relatively homogenous catches in mid-water trawls). And sure enough, when the net was brought up, I couldn’t believe my eyes!

All told, we sorted through over 7,000 animals, a total of 36 different species represented in the total catch. It took 4 of us over 4 hours to sort, measure, and weigh all these animals. There were over 350 walleye pollock in this catch as well as skates, octopi, crabs, snails, arrowtooth flounder, sea anemones, star fish, and dozens of other animals. Some of them were even walking themselves down the table.

During this catch, I also learned how to take the ear bones, or otoliths, out of a walleye pollock. Why ear bones you might ask? Using the ear bones from a walleye pollock, scientists are able to determine the exact age of the fish. Misha Stepanenko, one of the two Russian scientists on board the Oscar Dyson, showed me how to cut partially through the fish’s skull and take out two large ear bones. Once they were taken out, I put them in a solution to preserve them. Back in NOAA’s Seattle lab, the ear bones are stained, enabling scientists to count the different layers in each ear bone. For every year that the fish lives, a new layer of bone grows, similar to how trees add a layer for each year that they live. By learning the exact age of a fish, scientists are able to track age groups (called “cohorts”), allowing more precise modeling of the walleye pollock population life cycle.

A diagram of an otolith, or ear bone, of a fish. You can see that it’s a lot like looking at tree rings!
A diagram of an otolith, or ear bone, of a fish. You can see that it’s a lot like looking at tree rings!

Personal Log 

So far this trip, we have sailed within 15 miles of Cape Navarin (Russia) on at least two different occasions but fog and clouds prevented any glimpse of land both times. It was a frustrating feeling knowing that land was so close, yet impossible to see. After 12 days of looking at nothing but water and sky, seeing land would have been a welcome treat.

Despite not seeing land, I still felt like I was in Russia just from listening to different fishing vessels communicate with one another. On our first night in Russian waters, we sailed through a heavy fog, with 7 or 8 different boats fishing nearby. I was impressed with how Ensign Faith Opatrny, the Officer on Deck at the time, communicated with various vessels, using collision regulations (“the rules of the road”) to navigate safely. On a culinary note, I got my first chance to eat some of a catch. After most trawls, we discard remaining inedible specimens overboard. After our bottom trawl however, one of the scientists filleted some of the cod. The next day, the stewards cooked it up for lunch. It tasted great and it felt good to be eating some of the fish that we sampled.

A graph showing the adult walleye pollock biomass estimates from 1965 to 2008.
A graph showing the adult walleye pollock biomass estimates from 1965 to 2008.

As the cruise starts to wind down, I also want to express my gratitude to all the NOAA scientists and Oscar Dyson crew. Everyone in the science group took time to explain their research, teach me scientific techniques, and answer my many questions. On numerous occasions, the deck crew explained the mechanics of fishing nets as well as the fishing process. The engineering crew gave me a tour of the engine rooms, describing how four diesel engines power the entire boat. The survey techs explained how different equipment is operated as well as the information it relays back to the scientists. The NOAA Corps officers showed me how to read weather maps, take coordinates, and explained ship navigation. The ship’s stewards described the art and science behind feeding 33 people at sea. And the USFWS bird observers patiently showed me how to identify numerous bird species. From each of them, I learned a tremendous amount about fisheries science, fishing, boats, sailing, birding, and life in the Bering Sea. Thank you!

Answer to July 28 (Tuesday) Log: How has the walleye pollock biomass changed over time? 
In the past few years, the walleye pollock biomass has decreased (according to the acoustic-trawl survey, the survey that I joined.) It should be noted that there is a second complementary walleye pollock survey, the eastern Bering Sea bottom trawl survey. This survey studies walleye pollock living close to the sea floor. As walleye pollock age, they tend to live closer to the sea floor, thus the bottom trawl survey sometimes shows different biomass trends than the acoustic-trawl survey. Both surveys are used together to manage the walleye pollock stock.

An up-close look at one of the squid’s tentacles
An up-close look at one of the squid’s tentacles

Animals Seen 
Auklet, Arrowtooth flounder, Basket star, Bering skate, Cod, Hermit crab, Fin whale, Fur seal, Octopus, Sculpin, Sea mouse, Sea slug, Shortfin eelpout, Snow crab, Squid, and Tanner crab.

New Vocabulary: Bottom trawl – fishing conducted on and near the bottom of the sea floor. Catch – fish brought up in a net. Shoot the doors – a fishing expression that means to lower the 2 metal panels that hold open the fishing nets in the water. Stewards – the name for cooks on a ship. Table – nickname for the conveyor belt where the fish are sorted for sampling. Vessels – another word for ships. 

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Kathryn Lanouette, July 28, 2009

NOAA Teacher at Sea
Kathryn Lanouette
Onboard NOAA Ship Oscar Dyson
July 21-August 7, 2009 

Here I am sorting different zooplankton species
Here I am sorting different zooplankton species

Mission: Summer Pollock Survey
Geographical area of cruise: Bering Sea, Alaska
Date: July 28, 2009

Weather Data from the Ship’s Bridge 
Visibility: 8 nautical miles
Wind direction:  015 degrees (N, NE)
Wind speed:  7 knots
Sea wave height: 1 foot
Air temperature: 7.6˚C
Seawater temperature: 7.3˚C
Sea level pressure: 29.8 inches Hg and falling
Cloud cover: 8/8, stratus

Science and Technology Log 

In addition to studying walleye pollock, NOAA scientists are also interested in learning about the really tiny plants (phytoplankton) and animals (zooplankton) that live in the Bering Sea.  Plankton is of interest for a two reasons. First, phytoplankton are the backbone of the entire marine food chain. Almost all life in the ocean is directly or indirectly dependent on it. By converting the sun’s energy into food, phytoplankton are the building blocks of the entire marine food web, becoming the food for zooplankton which in turn feed bigger animals like small fish, crustaceans, and marine mammals. Second, zooplankton and small fish are the primary food source for walleye pollock. By collecting, measuring, and weighing these tiny animals, scientists are able to learn more about the food available to walleye pollock. In addition, every time the scientists trawl for walleye pollock, the stomachs of 20 fish are cut out and preserved. Back at a NOAA lab in Seattle, the contents of these fish stomachs will be analyzed, giving scientists a direct connection between walleye pollocks’ diet and specific zooplankton populations found throughout the Bering Sea.

A simplified marine food chain (Note: A complete marine food web involves hundreds of different species.)
A simplified marine food chain (Note: A complete marine food web involves hundreds of different species.)

Two important zooplankton groups in the Bering Sea are copepods and euphausiids (commonly referred to as krill). Euphausiids are larger and form thick layers in the water column. In order to catch euphausiids and other zooplankton of a similar size, a special net called a Methot is lowered into the water. This fine meshed net is capable of catching animals as small as 1 millimeter. The same sonar generated images that show walleye pollock swimming below the water’s surface are also capable of showing layers of zooplankton. Using these images, the scientists and fishermen work together, lowering the net into the zooplankton layers.

The Methot net is the square shaped net in the background. It was just brought up and is filled with hundreds of zooplankton.
The Methot net is the square shaped net in the background. It was just brought up and is filled with hundreds of zooplankton.

Once the Methot net is back onboard the boat, its contents are poured through fine sieves and rinsed. All species are identified. A smaller sub sample is weighed and counted. This information is applied to the entire catch so if there were 80 krill, 15 jellyfish, and 5 larval fish in a sub sample, then scientists would approximate that 80% of the entire catch was krill, 15% was jellyfish, and 5% was larval fish. Having only seen photos of some of these zooplanktons, it was interesting to hold them in my hands and look at them up close. They seemed better suited for space travel or a science fiction movie than the Bering Sea!

Personal Log 

The day before, I caught my first glimpse of Dall’s porpoises. This pod of porpoises came swimming alongside the boat. It was awesome to see their bodies rise and fall in the water. I was surprised at how quickly they were swimming, darting in and out of the Oscar Dyson’s wake. Today, I also got my first glimpse of a whale! It was a fin whale, a type of baleen whale, about 20 meters from the boat. It was exciting to watch such a large mammal swimming in such a vast expanse of water. I’m hoping to see a few more marine mammal species before we return to port. The seas have been very calm for the last five days, at times as smooth as a mirror. I’m surprised that I’ve gotten used to falling asleep in the early morning hours and waking around midday. Now that I’ve adjusted to the 4pm to 4am shift, I’m wondering how strange it will be to return to my regular schedule back on the east coast.

Answer to July 25th Question of the Day: Why are only some jellyfish species capable of stinging? 
As I picked up my first jellyfish in the wet lab (asking at least twice “Are you sure this won’t sting?”), I wondered why some jellyfish don’t sting.  So I did some reading and asked some of the scientists a few questions. Here is what I found out: All jellyfish (called “gelatinous animals” in the scientific world) have stinging cells (nematocysts) in their bodies. When a nematocyst is touched, a tiny barb inside fires out, injecting toxin into its prey.  It seems that in some jellyfish, the barbs are either too small to pierce human skin or that nematocysts don’t fire when in contact with human skin.

One euphausiid and two different species of hyperiid amphipod (They are between 1-3 cm long)
One euphausiid and two different species of hyperiid amphipod

Animals Seen 
Capelin, Dall’s porpoise, Euphausiid, Fin whale, Hyperiid amphipod, and Slaty-backed gull.

New Vocabulary: Baleen whale – a whale that has plates of baleen in the mouth for straining plankton from the water (includes rorqual, humpback, right, and gray whales). Methot net – a square framed, small meshed net used to sample larval fish and zooplankton. Phytoplankton – plankton consisting of microscopic plants. Plankton – small and microscopic plants and animals drifting or floating in the sea or fresh water. Trawl – to fish by dragging a net behind a boat. Zooplankton – plankton consisting of small animals and the immature stages of larger animals

Question of the Day: How has the walleye pollock biomass changed over time?

 

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Jennifer Fry, July 27, 2009

NOAA Teacher at Sea
Jennifer Fry
Onboard NOAA Ship Miller Freeman (tracker)
July 14 – 29, 2009 

Mission: 2009 United States/Canada Pacific Hake Acoustic Survey
Geographical area of cruise: North Pacific Ocean from Monterey, CA to British Columbia, CA.
Date: July 27, 2009

The CTD, resembling a giant wedding cake constructed of painted steel, measures the composition of the water, salinity, temperature, oxygen levels, and water pressure.
The CTD, resembling a giant wedding cake constructed of painted steel, measures the composition of the water, salinity, temperature, oxygen levels, and water pressure.

Weather Data from the Bridge 
Wind speed: 13 knots
Wind direction: 003°from the north
Visibility: clear
Temperature: 13.6°C (dry bulb); 13.2°C (wet bulb)
Sea water temperature: 15.1°C
Wave height: 1-2 ft.
Swell direction: 325°
Swell height: 4-6 ft.

Science and Technology Log 

Each night beginning at around 9:00 p.m. or 21:00, if you refer to the ship’s clock, Dr. Steve Pierce begins his research of the ocean. He is a Physical Oceanographer and this marks his 11th year of conducting CTD, Conductivity, Temperature, and Density tests.

It takes 24 readings per second as it sinks to the seafloor. The CTD only records data as it sinks, insuring the instruments are recording data in undisturbed waters. For the past 11 years Dr. Pierce and his colleagues have been studying density of water by calculating temperature and salinity in different areas of the ocean. By studying the density of water, it helps to determine ocean currents. His data helps us examine what kind of ocean conditions in which the hake live. Using prior data, current CTD data, and acoustic Doppler current profiler, a type of sonar, Dr. Pierce is trying to find a deep water current flowing from south to north along the west coast.  This current may have an effect on fish, especially a species like hake.

This map illustrates part of the area of the hake survey.
This map illustrates part of the area of the hake survey.

Dr. Steve Pierce reminds us, “None of this research is possible without math. Physical oceanography is a cool application of math.” Another testing instrument housed on the CTD apparatus is the VPR, Visual Plankton Recorder.  It is an automatic camera that records plankton, microscopic organisms, at various depths.  The scientists aboard the Miller Freeman collect data about plankton’s feeding habits, diurnal migration, and their position in the water column.  Diurnal migration is when plankton go up and down the water column to feed at different times of day (see illustration below).  Plankton migration patterns vary depending on the species.The scientists aboard the Miller Freeman followed the east to west transect lines conducting fishing trawls. The first one produced 30 small hake averaging 5 inches in length.  The scientists collected marine samples by weighing and measuring them.

Dr. Steve Pierce at his work station and standing next to the CTD on a bright sunny day in the Northern Pacific Ocean.
Dr. Steve Pierce at his work station and standing next to the CTD on a bright sunny day in the Northern Pacific Ocean.
This illustration depicts the diurnal migration of plankton.
This illustration depicts the diurnal migration of plankton.

Personal Log 

It was extremely foggy today.  We traversed through the ocean evading many obstacles including crab and fishing buoys and other small boats.  Safety is the number one concern on the Miller Freeman. The NOAA Corps Officers rigorously keep the ship and passengers out of harm’s way.  I am grateful to these dedicated men and women.  LTjg Jennifer King, marine biologist and NOAA Corps officer says, “Science helps understand natural process: how things grow and how nature works. We need to protect it.  Science shows how in an ecosystem, everything depends on one another.”

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Jennifer Fry, July 26, 2009

NOAA Teacher at Sea
Jennifer Fry
Onboard NOAA Ship Miller Freeman (tracker)
July 14 – 29, 2009 

Mission: 2009 United States/Canada Pacific Hake Acoustic Survey
Geographical area of cruise: North Pacific Ocean from Monterey, CA to British Columbia, CA.
Date: July 26, 2009

Weather Data from the Bridge 
Wind speed: 10 knots
Wind direction: 100° [from the east]
Visibility: fog
Temperature: 13.5°C (dry bulb); 13.5°C (wet bulb)
Sea water temperature: 10°C
Wave height: 1ft.
Swell direction: 315° Swell height:  6 ft.

Here I am checking HAB samples.
Here I am checking HAB samples.

Science and Technology Log 

We conducted a number of HAB, Harmful Algal Bloom sample tests. The Harmful Algal Bloom test takes samples at predetermined location in our study area. The water is filtered to identify the presence of toxic plants (algae) and animals (zooplankton). The plankton enter the food chain specifically through clams and mussels and can be a possible threat to human health.

We also conducted XBTs, Expendable Bathythermograph; and one  fishing trawl net. The trawling was successful, catching hake, squid, and Myctophids.  Fishery scientist, Melanie Johnson collected specific data on the myctophids’ swim bladder.  The swimbladder helps fish regulate buoyancy.  It acts like a balloon that inflates and deflates depending on the depth of the fish. Sharks on the other hand have no swim bladder. They need to swim to maintain their level in the water. Marine mammals such as dolphins and whales have lungs instead of a swimbladder.  Most of the sonar signal from the fish comes from their swimbladder.  The study of the swimbladder’s size helps scientists determine how deep the fish are when using the sonar signals and how strong their sonar signal is likely to be.

Commander Mike Hopkins, LTjg Oliver Brown, and crewmember John Adams conduct a marine mammal watch on the bridge before a fishing trawl.
Commander Mike Hopkins, LTjg Oliver Brown, and crewmember John Adams conduct a marine mammal watch on the bridge before a fishing trawl.

The scientists tried to conduct a “swim through” camera tow, but each time it was aborted due to marine mammals in the area of the net. During the “Marine Mammal Watch” held prior to the net going in the water, we spotted humpback whales. They were observed breeching, spouting, and fluking. The humpback then came within 30 feet of the Miller Freeman and swam around as if investigating the ship.

Animals Seen Today 
Fish and animals trawled: Hake, Squid (Cephalopod), and Myctophids.
Marine Mammals: Humpback whale.
Birds: Albatross, Fulmar, and Shearwater.