fisheries – Page 5 – NOAA Teacher at Sea Blog

May 22, 2012August 11, 2021

Ellen O’Donnell: There’s a Lot of Food in the Ocean and One More Whale to Feed! May 20, 2012

NOAA Teacher at Sea
Ellen O’Donnell
Onboard NOAA Ship Delaware II
May 14 – May 25, 2012

Mission: North Atlantic Right Whale Survey
Geographical area of the cruise: Atlantic Ocean; Franklin Basin
Date: May 20, 2012

Weather Data from the Bridge: Light winds, slightly overcast, ocean swells between 3 to 5 feet.

Science and Technology Log:

We spent the night out at sea and today and we worked the Franklin Basin. It is about 120 miles from Cape Cod. At first we didn’t see many whales, but things started picking up by lunchtime. We launched the little gray boat shortly after to get close to the right whales we were seeing. While I didn’t go on the gray boat today, many of the whales came right up to the ship. It was another amazing day and we were quite successful.

copepod maine — Copepod (photo: at-sea.org)

I have seen so many different ways that the whales catch their prey. I asked the question last time, “Why do sei and right whales often appear together?” This is because they like the same food. Both whales eat copepods. Copepods are tiny crustaceans that range from microscopic to a quarter of an inch. Crustaceans are invertebrates which are related to lobster, shrimp and crabs. They eat diatoms and plankton, which are even smaller! They are the most abundant species on earth and are important in many ocean food webs.

Cool Fact from the Monterey Bay Aquarium: A single copepod may eat from 11,000 to 373,000 diatoms in 24 hours!

So sei and right whales feed on these tiny abundant organisms, which is amazing given their size. Humpbacks and fin whales also filter feed, but they eat krill (another tiny crustacean), plankton and small fish. Humpbacks can consume up to 3,000 pounds of food a day.

Sei and right whale feeding in same area (photo: Genevive Davis)

All of these whales are called baleen whales because they filter their prey out of the water as they move through it. Right whales and sei whales surface feed a lot. They are close to the surface slowly moving through the water filtering out copepods. Often they are seen feeding side by side.

Sometimes right whales do what is called echelon feeding. One whale is up front and then whales along each side create a V-shape. The whales to the side of the one in front pick up prey that didn’t make it into the forward whale’s mouth. We saw a great example of echelon feeding right from the ship. There were six right whales slowly swimming in this V-shape. Every once in a while, if one got out of formation, they would swim back toward the V and turn and get back in formation.

Humpback whales also use a method for catching prey. When we got close to the humpback, Slumber, the other day, we noticed large bubbles rising to the surface. This is called bubble feeding. Humpbacks create large bubbles to trap and herd fish. Often they do this in groups.

Mother and new calf (photo: Jenn Gatzke)

So while watching the different whales, and how they feed was very interesting, this was not the most exciting thing. These surveys are important because they keep track of vital information needed to develop good conservation plans. Therefore, information such as where the individual whales are, which females breed, where they breed, and how many calves are born is important.

We identified around 17 whales yesterday and found one that one had not been biopsied. This whale was then biopsied so its information can go into the database. We also saw two mothers and their calves. Right whales typically give birth to their calves after a 12 month gestation period, off the coast of Georgia or North Florida.

This year only six calves were born and one died. This number is not good as biologists hope to have the number of calves born in the double digits. So you can imagine how happy everyone was when we identified a female who hadn’t been seen since 2010 with a new calf! We were able to get a biopsy from the calf as well, which will not only give genetic information from the skin, but also information on contaminants from the mother since it is still nursing. But I’m not finished yet! The icing on the cake was that the baby whale also released some fecal matter. Yes that’s right…whale poop! This may not seem important to you, but the whale biologists were ecstatic. The collected whale poop, yes it was collected in a bucket, gives a wealth of information, such as what it has been eating and the level of contaminants in the calves body. Adult whale poop also gives hormonal information. All in all it was a very successful day of collecting important data on right whales.

DSCN2803 — Relaxing after a hard day’s work

: NOAA Scientists Peter Duley and Allison Henry scoop whale poop into a collection bag to be later analyzed

Personal Log

NOAA is an agency that enriches life through science. Their reach goes from the surface of the sun to the depths of the ocean floor as they work to keep citizens informed of the changing environment around them. Obviously the ocean is a big part of our environment. NOAA vessels have differing focuses on the data they collect from the ocean. The Delaware II is a fisheries vessel. It goes out on various research cruises, which collect data on different organisms within our oceans. As you know they perform right whale cruises, like the one I am on now, but they also perform other studies as well. Midwater trawling is done for studies on herring. Large nets are pulled along the boat at mid-water level, and the data collected gives information on the distribution and abundance of herring. Deep water trawls with nets are done to collect scallops and clams, and determine their relative abundance and distribution. Shark cruises collect sharks by sending out a line with baited hooks. The sharks collected are tagged and released. Lastly, the Delaware II performs ichthyoplanktic studies, which collect eggs and larvae from various species of fish.

DSCN1991 — Jim Pontz (left) and Todd Wilson (right) getting the trawl net ready (photo: Delaware II)

DSCN2016 — Herring catch (photo: Delaware II)

Clam and Scallop Survey (photo: Delaware II)

Shark Tag and Release Survey (photo: Delaware II)

It is the deck crew that helps make this possible. Acting Chief Boatswain and Head Fisherman, Todd Wilson heads up a 5-man crew, who not only take care of all ship maintenance, with the exception of the engine, but serve as night-time lookouts, and operators of the fisheries equipment. We rely on them to get the little gray boat in and out of the water, which takes a lot of coordination, and they are always there to help you if you need it.

DSCN2728 — Launching the little gray boat

August 30, 2011April 28, 2021

Kevin Sullivan: Baring the Bering, August 28, 2011

NOAA Teacher at Sea
Kevin C. Sullivan
Aboard NOAA Ship Oscar Dyson
August 17 — September 2, 2011

Mission: Bering-ALeutian Salmon International Survey (BASIS)
Geographical Area: Bering Sea
Date: August 25-28, 2011

Weather Data from the Bridge
Latitude: 56.95N
Longitude: 162.93 W
Wind Speed: 10 Knots
Surface Water Temperature: 10.5 C
Air Temperature: 55F
Relative Humidity: 97%

Science and Technology Log

My attempt at play on words for the title: “Baring the Bering”…… somewhat fitting as what we have been doing is literally trying to uncover and expose the hidden truths and secrets that this sea has to offer. I have become more comfortable with the scientific terminology being used on board and also have gotten into a nice flow with the overall processes going on and with the actual procedures and techniques being utilized to conduct these investigations. In the last blog entry, I was discussing the work I was doing alongside the oceanographers. I have been continuing this work and adding additional learning outcomes each day as this team throws more and more learning opportunities my way.

For example, yesterday we were dealing with primary productivity. This study is essentially trying to determine the rate at which photosynthesis is occurring. The amount of Phytoplankton–autotrophs (Self-feeders) obtaining their energy from sunlight–varies in different ecosystems as well as over time. For example, for the school where I teach, Sandy Hook, NJ is a nearby coastal estuarine system. Being an estuary and at mid-latitude, we have very high nutrient levels compliments of river runoff (in fact, excess runoff leads to algal blooms…think of it as pouring liquid Miracle-Gro into the waters and the resulting bloom that would occur. In the end, unfortunately, it leads to eutrophication, decrease in O2 and potentially fish kills) as well as strong sun angle. Therefore, we have large availability of productivity and biomass. The Bering Sea also has tremendous productivity and therefore biomass as well. Here, the relatively shallow seas of the Bering allow the Phytoplankton to transfer solar energy into chemical energy within the photic zone (area in which sun can penetrate). This coupled with the upwelling of nutrients off the shelf-break create the base of the food chain within these valuable, productive fisheries. There is still a lot of uncertainty as to the transport and fate of this setup but it is clear that we need to learn more and concentrate our efforts into putting these pieces together.

So, the actual procedure is to again take water from the CTD’s (explained in last Blog) Niskin Bottles at various depths and then “feed” these marine plants nutrients and give them there other ingredient to conduct photosynthesis, which is sunlight (they are already in H2o). We then take these samples and put them into a tank which is on the deck of the boat and has continuously circulating water. We also put on Mesh Nylon bags to mimic the light concentration from the various depths they were taken from. So for example, a sample taken at surface or near surface may be left without coverage whereas a sample taken at 50 meters may have two bags over the bottle and scatter the light entering to be representative of the light conditions the sample came from. In the picture below, you can see this tank, the bottles under experiment (the gray bottle in lower left is one with a mesh bag for light reduction and the dark bottle in the lower right allows no light through and is the control) and the continuous water circulating output in the lower right hand of the tank.

Now, the cool part of this, is that the nutrients that we introduced to the sample have been “laced” by stable isotopes of Carbon and Nitrogen. This way, after the sample has been filtered and the chlorophyl analyzed, we can make certain assumptions about how productive these phytoplankton are based on the isotope markers.

I cannot emphasize the importance of these producers enough. Think of them as being the base of a pyramid (which is often used by ecologists) — if they are removed, all of the other trophic (feeding) levels cannot exist. It takes a tremendous amount of producers to feed fewer and larger carnivores. This has to do with a rule in Ecology/Biology refered to as the “10% rule”. We cover this in class and will review it in more detail. In the interim, check out this website for pre-reading information on the flow of energy in an ecosystem.

I often cite the following excerpt in class to illustrate this concept:

“Three hundred trout are needed to support one man for a year. The trout, in turn, must consume 90,000 frogs, that must consume 27 million grasshoppers that live off of 1,000 tons of grass.”
—
G. Tyler Miller, Jr., American Chemist (1971)

Ok, so for the next few blogs, I will start to debrief my followers on my experiences aboard the Oscar Dyson as they relate to the Fisheries end of this cruise and tie it into the Oceanographic studies I have spent the last few entries explaining. I figured it made most sense to start at the base of the food chain and make my way up to the higher ordered species and then summarize with the interactions of all components for the Bering Sea and in turn, our global sea that represents 97% of all of Earth’s water supply.

In the interim, check out Where I am, almost real-time HERE. From this site, you can obtain current latitude/longitude, wind speed, water temp etc.

Personal Log

As I noted in the last blog, Hurricane Irene was a real threat to the East Coast and NOAA’s “Hurricane Hunters” (see last blog entry) did an excellent job at keeping the public informed about the status of the storms strength, location, and traveling direction. I brought it up last entry to illustrate the depth and scope of NOAA as an organization. Now that she has come and left her mark, lets take it one step further. Many places in the Mid-Atlantic received over 10″ of rain. Can you name two major river basins along the East Coast that drain into the Atlantic Ocean? If this water travels over millions of people’s yards (that have been heavily fertilized), and farming areas with livestock, think of the nutrient input into the Atlantic Basin. Relate this to the work currently being done on the Oscar Dyson. Remember, that off our coast of NJ, we often have to worry about an influx of too many nutrients and algal blooms…..If you want to learn more about causes/effects, then read this website about eutrophication.

During our travels yesterday, we were just offshore of very remote Cape Newenham, Alaska. I took the following picture. At the top of this mountain you can make out a white structure. This was part of a system titled “White Alice Communication Systems” which was a “US Air Force telecommunication link system constructed in Alaska during the Cold War. It also connected remote Air Force sites in Alaska such as Aircraft Control and Warning (AC&W), Distant Early Warning line (DEW Line) and Ballistic Missile Early Warning System (BMEWS). The system was advanced for its time, but became obsolete within 20 years following the advent of satellite communications.” (http://en.wikipedia.org/wiki/White_Alice_Communications_System)

August 26, 2011April 28, 2021

Kevin Sullivan: Bering Sea Bound, August 22, 2011

NOAA Teacher at Sea
Kevin C. Sullivan
Aboard NOAA Ship Oscar Dyson
August 17 — September 2, 2011

Mission: Bering-ALeutian Salmon International Survey (BASIS)
Geographical Area: Bering Sea
Date: August 22-24, 2011

Weather Data from the Bridge
Latitude: N
Longitude: W
Wind Speed: 20-23kts Tue,Wed. seas 9′ Thu 8/25 = calm
Surface Water Temperature: C
Air Temperature: 55F
Relative Humidity: 70%

Science and Technology Log

We are on Day II of our travels to get to our first sampling station located in the SE Bering Sea. We will begin our fishing operations today! We have had decent weather thus far although we did just go through Unimak Pass (see picture below of location) which is a narrow strait between the Bering Sea and the North Pacific Ocean. This passage offered a time of heavier seas. I’m guessing that like any strait, the currents may become more funneled and the seas “confused” as they squeeze through this area. It’s kind of analogous to it being more windy in between buildings of a major city vs. suburbia as the wind is funneled between skyscrapers. I also imagine this to be a popular crossing for marine mammals as well.

Interesting to think that both marine mammals and humans use this passage to both get to the same things: a food source and a travel route. It’s a migratory “highway” for marine mammals, and a heavily-trafficked area for humans in international trade and commercial fisheries.

Anyway, the Bering Sea is a very unique body of water. It really is the way that I imagined it. It is as though you are looking through a kaleidoscope and the only offerings are 1000 different shades of grey. It is rainy, foggy, and windy. I can appreciate how this sea has been the graveyard for so many souls and fishing vessels in the past who have tried to extract the bounties it has to offer.

As of Wednesday, the 24th, we have finished 4 stations of the 30 that have been planned for Leg I of this study (Leg II is of similar duration and goals). I was involved with helping the oceanographic crew with their tasks of collecting and evaluating various parameters of water chemistry. To do this, an instrument called a “CTD”– an acronym for Conductivity, Temperature, and Depth — is lowered. This instrument is the primary tool for determining these essential physical properties of sea water. It allows the scientists to record detailed charting of these various parameters throughout the water column and helps us to understand how the ocean affects life and vice-versa.

One aspect that I found very interesting is the analyzing of chlorophyll through the water column. All plant life on Earth contains the photosynthetic pigment called chlorophyll. Phytoplankton (planktonic plants) occupy the photic zone of all water bodies. Knowing that we live on a blue planet dominated by 70% coverage in water, we can thank these phytoplankton for their byproduct in photosynthesis, which is oxygen. Kind of strange how you often symbolize the environmental movement with cutting down of the rainforests and cries that we are eliminating the trees that give us the air we breath. This is true, but proportionately speaking, with an ocean-dominated sphere, we can thank these phytoplankton and photosynthetic bacteria for a large percentage of our oxygen. Additionally, being at the base of the food chain and primary consumers, these extraordinary plants have carved a name for themselves in any marine investigation/study.

The procedure to measure chlorophyll involves the following: water from the Niskin Bottles (attached to the CTD, used to “capture” water at select depths) is filtered through different filter meshes and the samples are deep-frozen at -80F. To analyze chlorophyll content, the frozen sample filter is immersed in a 90% solution of DI (Distilled Water) and acetone which liberates the chlorophyll from the phytoplankton. This is then sent through a fluorometer.

Filtering water from CTD for Chlorophyll Measurements

Fluorescence is the phenomena of some compounds to absorb specific wavelengths of light and then, emit longer wavelengths of light. Chlorophyll absorbs blue light and emits, or fluoresces, red light and can be detected by this fluorometer.

Amazing to think that with this microscopic plant life, you can extrapolate out and potentially draw some general conclusions about the overall health of a place as large as the Bering Sea. Oceanographic work is remarkable.

Personal Log

The crew aboard the Oscar Dyson have been very accommodating and more than willing to educate me and take the time to physically show me how these scientific investigations work. I am very impressed with the level of professionalism. As a teacher, I know that most often, the best way to teach students is to present the material in a hands-on fashion…inquiry/discovery based. This is clearly the format that I have been involved in while in the Bering Sea and I am learning a tremendous amount of information.

The food has been excellent (much better than I am used to while out at sea). The seas have been a bit on the rough side but seem to be settling down somewhat (although, I do see a few Low Pressure Systems lined up, ready to enter the Bering Sea…..tis the season). Veteran seamen in this area and even in the Mid-Atlantic off of NJ, know that this is the time of year when the weather starts to change). On a side note, I see that Hurricane Irene has its eyes set on the Eastern Seaboard. I am hoping that everyone will take caution in my home state of NJ.

Lastly, it’s amazing also to think of the depth and extent of NOAA. With oceans covering 70% of our planet and the entire planet encompassed by a small envelope of atmosphere that we breathe, it is fair to say that the National Oceanic and Atmospheric Administration is a part of our everyday lives. I am in the Bering Sea, one of the most remote and harsh places this planet has to offer and across the country, there are “Hurricane Hunters” flying into the eye of a hurricane that could potentially impact millions of people along the Mid Atlantic………..Both operated and run by NOAA!

Sunset on the Berring Sea 08-24-11 — Sunset on the Bering Sea 08-24-11

June 28, 2011April 28, 2021

Tammy Orilio, Fisheries Acoustics, June 28, 2011

NOAA Teacher at Sea: Tammy Orilio
NOAA Ship Oscar Dyson
Mission: Pollock SurveyGeographical
Area of Cruise: Gulf of Alaska
Date: 28 June 2011

Weather Data from the Bridge:
Latitude: 57.11 N
Longitude: -155.58 W
Wind Speed: 3.61 knots
Surface Water Temp: 9.0 degrees C
Water Depth: 271.10 m
Air Temp: 8.3 degrees C
Relative Humidity: 84%

Science & Technology Log
Today we will look at the acoustic system of the NOAA Ship Oscar Dyson! Acoustics is the science that studies how waves (including vibrations & sound waves) move through solids, liquids, and gases. The Oscar Dyson uses an acoustic system to find the pollock that we process.

The process begins when a piece of equipment called a transducer converts an electrical pulse into a sound wave. The transducers are located on the underside of the ship (in the water). The sound travels away from the vessel at roughly1500 feet per minute, and continues to do so until the sound wave hits another object such as a bubble, plankton, a fish, or the bottom. When the sound wave hits an object, it reflects the sound wave, sending the sound wave back to the Oscar Dyson as an echo. Equipment onboard listens to the echo.

good fishing — An image of the computer screen that shows a great number of fish. This was taken underneath the boat as we were line fishing in Sand Point.

The computers look at two critical pieces of information from the returning sound wave. First, it measures the time that it took the echo to travel back to the ship. This piece of information gives the scientists onboard the distance the sound wave traveled. Remember that sound travels at roughly 1500 feet per minute. If the sound came back in one minute, then the object that the sound wave hit is 750 feet away (the sound traveled 750 feet to the object, hit the object, and then traveled 750 feet back to the boat).
The second critical piece of information is the intensity of the echo. The intensity of the echo tells the scientists how small or how large an object is, and this gives us an idea of what the sound wave hit. Tiny echos near the surface are almost certainly plankton, but larger objects in the midwater might be a school of fish.

poor fishing — The same spot as above, but with practically no fish.

One of the things that surprised me the most was that fish and bubbles often look similar enough under water that it can fool the acoustics team into thinking that the bubbles are actually fish. This is because many species of fish have gas pockets inside of them, and so the readout looks very similar. The gas pockets are technically called â€œswim bladdersâ€ and they are used to help the fish control buoyancy in the water.

Personal Log:

Well, it’s now Tuesday morning, and we are making excellent time on our way back to Kodiak. The water has not been as rough as expected, thank goodness! Yesterday’s forecast said we’d encounter winds up to 35 knots and seas up to 18 feet, but I have definitely not felt anything like that. It’s not quite over yet, though, so I’m not getting my hopes up too much.

We’re scheduled to arrive in Kodiak sometime tomorrow (I don’t know the approximate time yet), or maybe even later tonight, which means I’ll have a day to kill there. I’m looking forward to it because I didn’t get a chance to explore when I first arrived. When I made it to Kodiak, I only had the clothes on my back, and it was raining for nearly the entire two days I was there, so I didn’t want to go outside and explore because if my clothes got wet, I had nothing else to change into! One animal I haven’t seen on this trip is an eagle, and I hear they’re very easy to spot in Kodiak, so hopefully I’ll get a chance to look around tomorrow!

Question of the Day:

What is one way that bony fishes can control the amount of gas in their swim bladder?

June 2, 2010April 7, 2021

Laura Rodriguez, June 2nd, 2010

NOAA Teacher at Sea
Laura Rodriguez
Aboard NOAA Ship Oscar Dyson
May 24 – June 2, 2012

Mission: Fisheries Surveys
Geographical Area: Eastern Bering Sea
Date: June 2, 2010

Why is Ocean Science Important?

My cruise is coming to an end. We are now sampling the last of the stations as we make our way back to Kodiak. On Saturday, we had a safety stand down drill. This entailed finding a spot close to shore where we could drop anchor and then have a little bit of free time. Some people fished for halibut off the boat and others went ashore to explore a little bit. I went ashore with a group that included the XO, Jeff Shoup, Ensign Amber Payne, Glen Whitney, Dennis Boggs, and two of the scientists, Tiffany Vance and Kevin Bailey. We hiked around a part of Katmai National Park and Preserve. This is an area filled with active volcanoes and glaciers. We saw a brown bear and a fox.

Four-peaked-glacier — Four peaked glacier

We also saw a raft of sea lions close to shore that eventually came closer and told us to go away. Katmai Preserve is home to an estimated 2,000 bears. The area we visited is very remote with no roads leading to it. Once back on board, it was back to work sampling more stations.

My time on board the Oscar Dyson has shown me both the beauty of the ocean and the need for people to understand and care for it. We are inextricably connected to the ocean. Whether we live near or far from the ocean, we depend on the ocean for fresh water (think water cycle) oxygen (the majority of oxygen in our atmosphere is produced by the phytoplankton in the ocean), food, medicines, and mineral and energy resources. Many people depend on the ocean for jobs and recreation. Our oceans, however, are fragile ecosystems that are affected by the activities of humans. Dumping wastes into the ocean, overfishing, drilling for oil and development along coastal areas all have consequences for the living things that call the ocean home. I have learned about areas where overfishing has depleted species of fish that may never come back. There is an area in the Gulf of Mexico that is called the dead zone because of fertilizers from farms dumped into the Gulf from the Mississippi River. Right now, there is the Deep Horizons oil leak that has already spilled 20 million gallons of oil into the Gulf of Mexico and is leaking over 500,000 gallons of oil a day. We have a history of taking the ocean for granted and believing that it is so big that it can absorb unlimited amounts of pollution. We are finding out how wrong we are. Taking care of the ocean is everyone’s responsibility. In order to take care of the ocean, it is crucial that we understand the interrelationships between what we do here on land and what happens in the sea. This is why research such as what the scientists are doing on the Oscar Dyson is so important.

Answers to your questions:

Dan 1. – Radar is different from sonar. Radar uses radio waves, a form of electromagnetic radiation (light) to detect objects. Radar stands for radio detection and ranging. Sonar uses sound waves to detect objects. Sonar stands for sound navigation and ranging.

Dan 2. – The weather is not nearly cold enough to need the de-icers. I was, however, standing by one the other day and felt the warmth, so they are on.

Olivia – My classification on this cruise is officially “Teacher at Sea.” I am, however, included with the scientists.

Kylei – I have been very lucky with the weather. We have not had any bad weather. One day, the ocean had some pretty good swells and we were rocking and rolling a bit, but no real storm. It has actually been unusually sunny and mild here.

Your question to answer: Research one of the activities below that affects life in the ocean:

Overfishing ( factory fishing ships)
Whaling
Offshore oil Drilling
Ocean pollution
Coastal development

Find out:

Why are people concerned about this activity?
What are people doing to protect the ocean from the negative aspects of this activity?
What can you do to help protect the ocean and the life within it?