Robert Oddo, July 30, 2009

Posted on July 30, 2009 by Teacher at Sea

NOAA Teacher at Sea
Robert Oddo
Onboard NOAA Ship Ronald H. Brown
July 11 – August 10, 2009

Mission: PIRATA (Prediction and Research Moored Array in the Atlantic)
Geographical area of cruise: Tropical Atlantic
Date: July 30, 2009

Deploying a buoy

Weather Data from the Bridge
Outside Temperature 25.50^oC
Relative Humidity 87%
Sea Surface Temperature 25.75^oC
Barometric Pressure 1017.3 inches
Latitude 20 09.721 N Longitude 33 34.806 W

Science and Technology Log

On the 28^thof July we did our 34^thCTD and changed out our third buoy and started to steam west back towards the states. We have a break now from our 12-hour shifts and only have one more buoy to change out and only one more CTD to deploy. I wanted to write about a couple of things that I have noticed over the last couple weeks when sampling that I thought were noteworthy. The seawater we collect from 1500 feet down in the ocean, even though we are in the tropics, is still very cold. It is about 4 degrees C or 39 degrees F while the sea surface temperature is around 26 degrees C or 79 degrees F.

Nightly Science Seminar

Another thing that is really cool is that when we are doing CTDs at night the lights from the ship attract squid and you can watch the squid chasing flying fish at the surface. The last thing that is strange, is that every once in a while even though we are hundreds of miles away from land, a butterfly or dragonfly darts around the ship. You just wonder where they have come from. Every night around 8 pm, there is meeting of all the scientists onboard. We usually get a weather briefing and then someone will give a seminar on the work they are doing. There are many links between the work that each scientist is doing on this ship and this is an important way to share ideas, get feedback and create new questions.

Personal Log

There is down time on the ship and I wrote about the movies earlier. We have a ping-pong table set up in the main lab where we play in our spare time. Since we are so far from any land, safety is very important on the ship. We have fire drills and abandon ship drills weekly. After the drill there is a briefing and the safety officer discusses some of the safety equipment the ship has and its use. Today we went out to the fantail and the officers demonstrated how to use flares and smoke signals.

A little ping pong in the main lab (left) and flare demonstration (right)

Research cruise plan

Jennifer Fry, July 29, 2009

Posted on July 29, 2009 by Teacher at Sea

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 29, 2009

Weather Data from the Bridge (0800)
Wind speed: 10 knots
Wind direction: 345° from the north
Visibility: fog
Temperature: 14.1°C (dry bulb); 13.8°C (wet bulb)
Sea water temperature: 10.6°C
Wave height: 1 ft.
Swell direction: 320°
Swell height: 3-5 ft.
Air pressure: 1011.0 mb
Weather note: There are two temperature readings taken on the Miller Freeman. The dry bulb measures the current temperature of the air. The wet bulb measures the absolute humidity of the air; uses a thermometer wrapped in a wet cloth. The dry and wet temperatures together give the dew point and help to determine humidity.

Science and Technology Log

Those aboard the Miller Freeman: including NOAA Corps, crew, and scientists were randomly selected to answer the following question.

How are science and the environment important to the work you do?

Here are some of their responses:

Lisa Bonacci, Chief Scientist/Research Fish Biologist, M.S. Marine Biology
“As a Fisheries Biologist at NOAA I work in applied science. Our research provides information that managers and policy makers use to make important decisions at a national level. These decisions help the United States keep our fisheries sustainable and at the same time protect our ocean ecosystems.”

Pat Maulden, Wiper, Engineering Department
“I like being part of the solution. If you’re not part of the solution, you are part of the problem.”

John Pohl, NOAA Oceanographer, B.S. Oceanography
“Every action has a consequence. Science improves our understanding of the world around us and consequences of our actions in the natural world. We are not separate from the environment in which we live. We can’t hold ourselves out of the natural world, or we will affect the balance.”

Steve DeBlois, NOAA Research Fish Biologist
“Science is a methodology by which we understand the natural world.”

Jose Coito, Lead Fisherman
“I try to help the scientific research on the ship whenever I can. I enjoy my job.”

LTjg Jennifer King, NOAA Corps Officer, B.S. Marine Biology
“Science helps understand natural processes: how things grow, and how nature works. We need to help protect it. Science shows how in an ecosystem, everything depends on one another.”

Steve Pierce, Physical Oceanographer, Oregon State University, Ph.D. Physical Oceanography “None of this research is possible without math. My study is a cool application of math.”

John Adams, Ordinary Fisherman
“Science helps you understand why things go. The environment is really important to protect because it’s the only one we’ve got.”

LTjg Oliver Brown, NOAA Corps Navigation Officer, B.S. Geology
“Understanding the processes of today to predict and sustain the systems of tomorrow. Anything you can study: fisheries, atmospheric or any “ology”, the ocean plays a part in it.”

Adam Staiger, Second Cook
“Remember to clean up after yourself.”

Francis Loziere, Able Seaman, B.S. Chemistry/Engineering
“Studying science can help foster original thinking. We need original thinking to save the planet.”

Julia Clemons, Oceanographer, M.S. Geology
“Science helps us to better understand the world we live in so we are not ignorant and live in a more responsible and aware manner.”

Chris Grandin, DFO, Canadian Fisheries, Biologist, M.S. Earth & Ocean Sciences
“We’re here to keep tabs on the fish resources of our planet, to ensure that there will be fish for the future generations, and to sustain our ecology. We all need to take responsibility.”

Dezhang Chu, NOAA fisheries, Physical Scientist, PhD Geophysics
“To study science you need devotion and dedication. It’s not something you make a lot of money at, but you can contribute good things to human society.”

Gary Cooper, Skilled Fisherman,
“I’ve always loved the sea. You get out of a job, what you put into it. Set your goals high and you’ll be successful.”

Melanie Johnson, NOAA Fishery Biologist
“Taking care of our environment, it’s the right thing to do. We need to live responsibility and sustainably; we can’t over fish or litter our world. If you don’t want it in your backyard, don’t put it in the ocean.”

Mark Watson, Wiper, Engineering Department
“Life and science go hand in hand; you can’t have one other the other.”

Ed Schmidt, First Assistant Engineer, Relief Chief “In my field of engineering, science and math go hand in hand. You have to have both. n the science side, there are relationships between different fluids, gases, and the theories behind what make the equipment work. You need to use math to find combustion rates, horsepower, electricity produced/consumed, and the list goes on and on. Without math and science I wouldn’t have a job.”

Ed Schmidt, First Assistant Engineer, Relief Chief
“In my field of engineering, science and math go hand in hand. You have to have both. On the science side, there are relationships between different fluids, gases, and the theories behind what make the equipment work. You need to use math to find combustion rates, horsepower, electricity produced/consumed, and the list goes on and on. Without math and science I wouldn’t have a job.”

The engineers aboard the Miller Freeman are a group of hard working people. There are always engineers on duty 24 hours/ day to ensure the ship is running properly. Jake DeMello, 2^nd engineer, gave me a tour of the Miller Freeman’s engine room. Jake attended California Maritime Academy where he received his Bachelor of Science degree in Marine Engineering. He has a 12-4 shift which means that he works from noon to 4:00 p.m. and then again from midnight to 4:00 a.m.

Jake DeMello stands by the desalination machine in the Miller Freeman’s engine room.

Before taking the job aboard NOAA’s Miller Freeman, Jake worked on a Mississippi River paddle boat traveling from New Orleans north past St. Louis through the rivers’ many dams and locks. He reminisced on one memorable moment aboard the paddleboat; the day he saw Jimmy Dean, the famous singer and sausage maker. Jake and the other engineers do many jobs around the ship including checking the fuel and water levels throughout the day and fixing anything that needs repairing. The Miller Freeman is equipped with a machine shop, including lathe and welding equipment.

Among the jobs of the engineer is reporting daily fuel levels including:

Hydraulic oil used for daily fish trawls, CTD, gantry, and winch operations.
Gasoline used for the “Fast Recovery Boat.”
Diesel fuel used for the main engine.
Lube oil used for main engines and generators.

We say good-bye to the hake both big and small.

Fresh water production: The ship’s water desalination machine transforms 2,000 gallons of sea water into fresh drinking water daily. The ship’s water tanks hold a total of 7,350 gallons of fresh water. Another job of the engineer is taking soundings throughout the day/night. Taking soundings means measuring the levels of liquid in the tanks. There are tanks on both the starboard and port sides of the ship. The engineer needs to be sure that fuel levels are evenly distributed so that the ship will be evenly balanced in the ocean.

Vocabulary: Starboard: right side of the ship. Port: left side of the ship.

Personal Log

I write this off the coast of Oregon in the North Pacific Ocean. It has been an amazing 17 days aboard the Miller Freeman. I feel honored to have participated in NOAA’s Teacher at Sea program. It has truly changed the way I look at science in the classroom and has given be a better understanding of how scientists conduct research on a day to day basis in the field. I am excited to have made so many learning connections between the real world of scientific study and the elementary school science classroom. I thank NOAA, the Teacher at Sea program and the entire crew, NOAA Corps, and scientists aboard the Miller Freeman for this opportunity.

My profound gratitude goes out to the dedicated science team aboard the Miller Freeman for all they have taught me.

John Schneider, July 27-29, 2009

Posted on July 29, 2009 by Teacher at Sea

NOAA Teacher at Sea
John Schneider
Onboard NOAA Ship Fairweather
July 7 – August 8, 2009

Mission: FISHPAC
Geographical Area: Bering Sea
Date: July 27-29, 2009

Position
In transit to Bristol Bay, AK

Weather Data from the Bridge
Weather System: highly variable in the Bering Sea
Barometer: falling on the second day
Wind: Ranging from light and variable to 35 kts
Low Temperature: 7.0º C
Sea State: initially <1-2 feet up to 8 feet on the evening of the 29th

The sheet above shows legs 5-10 of FISHPAC in the Bering Sea, AK

What Is FISHPAC?

The Magnusen-Stevens Fisheries Conservation Management Act includes the broad designation of “Essential Fish Habitat” (EFH) as including myriad parameters which are to be considered for all life stages of the managed species. Included in them are bottom type, epifauna and infauna, grain size, and organic debris. Additionally, studies are to span the life cycles of those species. There is an enormous amount of historical data relating to commercial fisheries catches, but the data have not been assembled as a whole and screened for accuracy. Additionally, there has been virtually no search for correlations within the data. Dr. Bob McConnaughey is engaged in seeking correlations between bottom characteristics, managed species and sorting through extant records in the search for utilizing sonar data to anticipate species presence in the Bering Sea. The phrase I’ve heard is “using bottom characteristics as proxy for prey identification.” Earlier cruise results can be viewed here. It would take a long time to describe all that they do at the Alaska Fisheries Service Center, so what I highly recommend is that you spend a while at their site.

Science and Technology Log

SeaBoss on deck

In addition to searching for correlations between trawl catch data and bottom characteristics, Dr. McConnaughey and his team are trying to determine if sound data (Multi-beam Echo Sounders and Side Scan Sonar) can be used in anticipating what species will likely be present in a given area. There are 69 managed commercial species in Alaska alone, which represent an enormous proportion of the commercial US catch, and if technology and research can be gained here, it can conceivably be applied elsewhere. The Alaskan fisheries have also not been subjected to as much commercial fishing as, say, the coast of New England due to the remote, harsh and generally newly populated area which is Alaska. Commercial fishing here is, for the most part, less than 50 years old compared to the hundreds of years off the East Coast.

SeaBoss being deployed. It is suspended from the J-Frame and swung outboard. Tending the SeaBoss can be hazardous so crew members are tethered to the deck.

Alaska has over 45,000 miles of coastline, contains 70% of the United States continental shelf, and 28% of the Exclusive Economic Zone (a 200 mile legal designation) yet much of that area has never been properly surveyed. With the prospect of a warming climate and potential northerly relocation of commercially viable species, it is essential to document as much of this area as possible before long-term damage may be inflicted on it. In order to evaluate the EFH parameters, one of the tools the FISHPAC team uses to gather bottom samples is an apparatus called the SeaBoss (Sea Bed Observation System.)

SeaBoss on the way up–it can be seen as deep as about 5 to 10 meters

SeaBoss allows the team to gather a 0.1m² bottom sample, descending and forward looking video and still pictures taken just before it hits the bottom. SeaBoss gets deployed twice at each site. The first sample is brought up and dumped into a sieve with a 1mm grid size. It is then gently hosed off with seawater to clear away the inorganic materials and large particles. The remaining biomass is put into containers with formalin solution for 2 days and then put into an alcohol solution to prevent decay. Those samples will be quantified back in the lab in the Seattle area. With the second sample from roughly the same bottom area, samples are taken of the bottom material itself from the surface and from a couple of centimeters below the surface. These, too, will be quantitatively evaluated back in the lab for grain sizes present and the proportions of those grain sizes in the sample. For background information on the SeaBoss, go here.

Jim Bush in the bosun’s chair. Rick Ferguson (l) and Chief Bosun Ron Walker assisting.

Personal Log

Before we left Dutch Harbor, we took on fuel (about ¼ of a load – only 22,000 gallons!) We took on ship’s stores (food.) 100+ gallons milk, 25 cases produce, a couple hundred pounds of meat (beef, chicken, pork, lamb,) scores of loaves of bread, and numerous cases of ice cream as well as other things. It took several hours to stow it all away. We also took on about 10 pallets of scientific gear for the FISHPAC team. One of the more interesting scenes was watching AB Jim Bush rigging the A-Frame for deploying some of the equipment off of the fantail.

Questions for You to Investigate

Check out the web sites I listed, there’s some really cool stuff on them.

New Terms/Phrases

Biomass – organic matter created by living things epifauna – living animals on the surface of the bottom infauna – living animals in the bottom quantitatively – using numerical values

Ginger Redlinger, July 29–31, 2007

Posted on July 29, 2009 by Teacher at Sea

NOAA Teacher at Sea
Ginger Redlinger
Onboard NOAA Ship Rainier
July 15 – August 1, 2007

Mission: Hydrographic Survey
Geographical Area: Baranof Island, Alaska
Date: July 29–31, 2007

Weather log on the RAINIER. Data is gathered, then entered into a database.

The RAINIER started its work in South East Alaska in April of this year. Four months and hundreds of nautical miles later it was time to leave: Juneau, Ketchikan, Sitka, Baranof Island, and the Gulf of Esquibel. Three or four research boats were in the water everyday rain or shine, calm or rough water, gathering data. At night, crews’ maintained watch, reviewed data, and planned for the next day’s work. Equipment was checked to ensure everyone’s health and safety. Quality control ensured that the data gathered met NOAA’s expectations. Now it is time to end the Alaskan part of their work and move to their next working location.

While traveling from South Each Alaska to Washington I reflected on the most memorable parts of the journey. I immediately remembered the compliments from pleasure boaters and fishermen about NOAA’s work. Next I thought about the ease at which the crew safely delivered and returned their equipment and crew to and from the ship each day. Then I thought about the NOAA resources I learned about as I studied information about hydrography, technology, satellites, weather, and tides. And how could I not mention the food – it was great. Good food compensates for the sacrifice of being away from home for such a long time.

Water from the Fraser River (green) and the southern end of Georgia Strait waters.

There would be a short break between the end of this voyage and the start of the next, some would remain on the ship, and for others it meant being “at home” for the first time since April. This is part of the sacrifice that mariners, and those who explore the oceans make. As we traveled closer to home many off-duty crewmembers gathered on the fly deck to see home slowly approaching from the distance. They shared stories from the last four months and recalled the moments of laughter on “the big white ship.” After traveling through Canadian waters, around Vancouver Island and into Puget Sound, people began to gather in earnest of the desk. At first I thought it was because we were taking a picture for a “NOAA 200^thAnniversary Postcard from the Field,” but many remained on deck. Many were anxious for the first glimpse of their families and their homes. Many of their family members arrived at the Ballard Locks – waving and communicating their excitement about the reunions that would happen in a few short hours.

Mt. Rainier and Seattle in the distance.

The sun is setting as we traveled past the many marinas for all types of marine vessels, houseboats, and dry-docks. As we passed through crewmembers neighborhoods the fading sunlight was replaced with light shining in their eyes as they talked about the view from their windows, their favorite neighborhood haunts, and local treats that mean “home.” As we turn toward the waters that lead to downtown Seattle the crew on the fly deck is silent. The last embers of sunlight are reflecting on the downtown Skyline, it is spectacular. We turn away from downtown and travel through the Fremont Cut. Thank goodness for the navigational skills of this young and talented team – the water traffic from Seattle’s SeaFair was busy. Once we arrived at the NOAA Western Regional Center in Sand Point, CO Noll’s work was done. He had trained his crew to successfully navigate the ship and complete the mission. We are all home; the final navigational command is given.

Rear Admiral De Bow handing the Command Coin to Commander Noll

“All Engines Stop” “All Engines Stop, Aye. – All Engines Stopped” “Very Well.” Rear Admiral De Bow was on board to congratulate him, and pass the time-honored command coin.

I hate to admit it, but like a kid at camp leaving a new set of friends knowing that I most likely will not see many of them again, I feel sadness. The memories and lessons will remain. What a great adventure for a teacher, what a great experience for those who work on the ship, and what a great service provided to those who depend on navigation for commerce, recreation, and those who seek a greater scientific understanding of the earth and how it changes. I can’t wait to share it all with my students and colleagues!!!!

The Seattle skyline at night

Jennifer Fry, July 28, 2009

Posted on July 28, 2009 by Teacher at Sea

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 28, 2009

Map of the world showing longitude and latitude lines

Weather Data from the Bridge
Wind speed: 17 knots
Wind direction: 345° from the north
Visibility: 8 nautical miles /clear
Temperature: 16.8°C (dry bulb); 11.6°C (wet bulb)
Sea water temperature: 15.5°C
Wave height: 3-5 ft.
Air pressure: 1012.9 millibars
Weather note: Millibars is a metric unit used to measure the pressure of the air.

Science and Technology Log

Weather Instruments and Predicting Weather

Lt Oliver Brown, surrounded by navigational tools, and Fishery Scientist Steve DeBlois make observations on the bridge of the Miller Freeman.

Everything that happens out at sea is dependent upon the weather forecasts. Throughout history man has used a variety of instruments to acquire accurate weather information. The Miller Freeman is equipped with state of art weather reporting instruments. Every 3 hours weather data is sent to the National Weather Service to help predict the weather at sea. Once again accuracy in reporting data is paramount.

Global Position: The Miller Freeman has several methods by which to determine longitude and latitude, which is our position in the ocean or on land. There are 2 G.P.S. systems on the bridge, a magnetic compass, a gyro compass, and radar. These instruments help determine the ship’s position.

True north: The actual location of a point on the earth related to the north pole.

A Gyrocompass with cardinal headings including north, south, east, and west

Magnetic north: Caused by the magnetic pull on the earth. Magnetic north heading is different depending on where you are on the earth, for instance, Magnetic north in Oregon has a variation of 16.45°east from true north. Southern California has a variation of 13.3° east from true north.

Temperature: Measured by a thermometer, units used are Celsius. Dry bulb: Measures air temperature. Wet bulb: Uses a thermometer wrapped in a wet cloth. The dry and wet temperatures together give the dew point and help to determine humidity.

Wind Speed: Measured in knots using an anemometer, or estimated by using the Beaufort scale. The Beaufort scale uses observations of the sea surface, and the effects of wind on people or objects aboard ship to estimate the wind speed.

Wind Direction: Is measured by what direction in which the wind is coming.

Cloud Height/Type: Is measured visually.

Cloud Type: Is measured visually using a variety of names of clouds depending on their patterning and altitude.

Magnetic compass

Visibility: Is measured by estimating how much of the horizon can be seen.

Wave Direction: measured visually from the direction the wave comes.

Wave Height: The vertical distance between trough (bottom of the wave) and crest (top of the wave) and is usually measured in feet.

Swell Direction/ Height: Measured visually usually in feet.

Personal Log

I have enjoyed my time on the bridge of the Miller Freeman immensely. I have a better understanding of the weather instruments used onboard and am getting better at spotting whales and identifying birds. I want to thank the entire NOAA Corps Officers who have taught me so much about how navigation and weather work aboard the Miller Freeman.

Crewmember John Adams uses on-board weather instruments
to record hourly weather readings that are then sent to National
Weather Service.

An anemometer, which measures wind speed

Kathryn Lanouette, July 28, 2009

Posted on July 28, 2009 by Teacher at Sea

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

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.)

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.

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 25^th 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

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?

Jennifer Fry, July 27, 2009

Posted on July 27, 2009 by Teacher at Sea

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.

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 11^thyear 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.

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.

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.”

NOAA Teacher at Sea Blog

Monthly Archives: July 2009

Robert Oddo, July 30, 2009

Jennifer Fry, July 29, 2009

John Schneider, July 27-29, 2009

Ginger Redlinger, July 29–31, 2007

Jennifer Fry, July 28, 2009

Kathryn Lanouette, July 28, 2009

Jennifer Fry, July 27, 2009