Pollock Survey – Page 26 – NOAA Teacher at Sea Blog

April 23, 2005March 18, 2021

Jim Jenkins, April 23, 2005

NOAA Teacher at Sea
Jim Jenkins
Onboard NOAA Ship Miller Freeman
April 18 – 30, 2005

Mission: Pollock Survey
Geographical Area: Bering Sea
Date: April 23, 2005

Mr. Jenkins helps to retrieve a Calvets net

Weather Data

Latitude: 57, 37, 50 North
Longitude: 156, 02, 34
West Visibility: 8 Nautical Miles
Wind Direction: 161 Degrees
Wind Speed: 17 Knots
Sea Wave Height: 4-5 Feet
Swell Wave Height: 4-6 Feet
Sea Water Temperature: 4 Degrees C
Sea Level Pressure: 1001.5
Cloud Cover: Partly Cloudy

Science and Technology Log

Get the microscopes ready!

Early this morning, I helped out with dropping and pulling up Calvets nets. These nets collect fish eggs and other small life forms from the sea. Specimens collected are put in jars, preserved with formaldehyde and sent to labs for analysis. This is a quantitative sample, meaning that each test is designed to get a good idea of the amount of fish eggs in a specific amount of water. In this case, the test measures eggs in a 100 cubic meter area. Specimens are filtered through a screen to eliminate most of the water. Screens are then rinsed to make sure all the netted material goes into the specimen bottle.

You can see how big Peggy the Mooring is with Mr. Jenkins standing in front of it!

Knowledge of the amount of fish eggs present in water can help make predictions about the health of fish populations. It can also help fishermen plan for the future. This morning we ran an extra test and I collected the contents of the net to bring back to Mountain View Elementary. There were a lot of copepods and some tiny worms visible to the naked eye in our specimen. Other portions of the collected specimen were squirming with life, but I could not make them out with just my eye. Let’s make looking at this specimen under the microscope the first activity that we do when I return to school.

The mooring named Peggy that I wrote you about earlier went into the water this morning. This was a complicated procedure. A couple of hours were spent “building” a chain with all the instruments which hang down to the bottom below this mooring, All of the instruments needed to be bolted to specific lengths of chain with shackles. The assembly was done according to a diagram drawn in Seattle. The total length of all the chains and instruments joined together was 67 meters long. Instruments used to gather data on temperature, salinity and nitrate levels at various depths were attached.

Once the chain was assembled, the whole assembly was lowered into the ocean as the times that each instrument hit the water were recorded. One end of the chain was joined with a shackle to the mooring and it is ALMOST ready to go Peggy, the mooring, is so big that it was a complicated job to get it into the water. Two winches, several rope lines, a lot of communication and thinking were necessary to get it into the sea. About an hour after the process began, Peggy touched down lightly in the sea. A big cheer went up from everyone on the deck!

Finally, the anchor needed to be attached to the bottom of the chain and dropped into the water. In this case, the anchor was not the railway wheels that you have heard about so often. This anchor resembled half of a Tootsie Roll Pop lying round side up and it was bright yellow. The exterior was made of concrete. A big mooring needs a big anchor! The anchor for Peggy weighed in at 5,000 pounds! (This is equivalent to 2 and one-half small cars).

How did an anchor this big get from the deck into the water? Again, it took considerable thinking and communication between deck hands and scientists. Communication between people on the deck and officers on the bridge was also extremely important so that the ship was in the right location. The cooperation, thinking and communicating paid off. Finally, Peggy the mooring, settled into the sea!

I took many photographs of the process of putting the mooing into the sea as well as a farewell photograph as the ship pulled away. These will be sent to you later today and will be there by Monday when you return to school.

By the way, another small mooring was put in right after lunch. Now we have an 18hour transit before reaching the site of deployment of the marine mammal listening device brought up by Chris Garsha and Lisa Munger that we discussed earlier.

Personal Log

I hope you guys had a great weekend!

Did you receive the photo of Rusty the ship’s cat? Well, I also sent copy of the photo to my home. My wife, Chantel, just wrote to advise that our son, Sam, climbed up in her lap when he saw the photo on the computer screen to give a big kiss to both his dad and to Rusty. Needless to say, this was a heartwarming message for me!

Question of the Day: What is at the center of the yellow concrete anchor used for the mooring named Peggy? (Hint: Reading previous logs might help you with this answer.) This “easy as candy” question comes to you in honor of the weekend! (Very Big Grin!)

April 22, 2005March 18, 2021

Jim Jenkins, April 22, 2005

NOAA Teacher at Sea
Jim Jenkins
Onboard NOAA Ship Miller Freeman
April 18 – 30, 2005

Mission: Pollock Survey
Geographical Area: Bering Sea
Date: April 22, 2005

Weather Data

Latitude: 56, 28, 22 N
Longitude: 160, 35, 21 W
Cloud Cover: Cloudy
Visibility: 6 Nautical Miles
Wind Direction: 164
Wind Speed: 20 Knots
Sea Wave Height: 3-4 Feet
Swell Wave Height: 2-3 Feet
Sea Water Temperature: 2.4 Degrees C
Barometric Pressure: 1011 MB

Science and Technology Log

How is visibility determined? This was the question I posed to Ensign Mandy Goeller. Her answer was that the distance is 10 nautical miles if the viewer can see the horizon. Distance may also be ascertained if another vessel shows up on radar and can also be seen with the eye. Finally, there is a degree of intuitive thought based on experience when writing visibility in a ships log.

A CTD cast was done this morning. This involves having a winch lower a huge instrument (about the size of motorcycle) into the water until it is almost resting on the bottom. Salinity, temperature and density readings are done on the way down for the instrument. Readings done on the way up would involve taking readings on water which has been disturbed by the passage of the instrument.

This morning’s reading was done for the benefit of The Kodiak Crab Lab (I bet you like that name!) in Kodiak, Alaska. One of the problems for king crab fishermen is that king crabs do not like to inhabit bands of cold water that stream through sections of the Bering Sea. Fishermen armed with knowledge of the location of these cold streams will likely not waste time, fuel and labor trying to catch crabs when the crabs are probably not going to be in the cold streams. NOAA is trying to help by supplying knowledge.

Retrieval of a mooring was scheduled for this morning. The boat arrived at the latitude and longitude at which the mooring was dropped off. A hydrophone (listening device attached to an electrical cord) was dropped into the water to listen for the device after a NOAA scientist sent it a signal to “wake up” and respond with a signal so that it could be located. The plan was to have an “acoustic release” sent to the mooring when it could be located. This signal would cause a metal latch located just above the anchor to open so that the mooring could rise to the surface, be spotted and be recovered. Unfortunately, the mooring never sent a signal. The acoustic release signal was sent but the mooring did not pop to the surface as planned. The mooring appears to be lost! I think it would be good to remember this the next time things do not go exactly as planned in our daily lives. Sometimes in science, as in all areas of human endeavor, things just do not go as planned.

The location of the lost mooring remains on file. Maybe it will be found in the future. Meanwhile, a mooring scheduled to be placed within a one third mile distance from the lost mooring was deployed as planned.

A second mooring was recovered as planned later in the day. This one was covered with huge barnacles and had a few life forms holding onto its surface. I took a few photographs of tiny crabs and worms which were found on this mooring. I held the crabs and worm in my hand for photographing so that you would have an idea of their size. I am thinking all the research you did on crabs before the trip may make it possible for you to identify the crab. Identifying the worm could be fun for someone!

Speaking of photos, I sent a number of photos to you today. Earlier, I had a problem with the size of files being too large to be sent by satellite to you. Please let me know what you think about the photographs.

Personal Log

I had breakfast this morning with Shawn Bowman, a young man wearing a Kings Point rugby shirt. Our conversation turned to rugby and I talked about one of our neighbors, Tom Levac, who is a student at The Merchant Marine Academy and also a rugby player. It turns out that Shawn is a graduate of the Merchant Marine Academy and played rugby with Tom. It is indeed a small world, isn’t it?

Had some time this morning just to walk around the deck and enjoy the beauty of the snow-capped peaks gracing coastal Alaska. This was a scene so beautiful that it was almost painful (You may not understand this at your stage in your life, but I bet that your parents will be able to tell you of a similar place. I was surprised when the people I was talking with when I described the beauty as being almost painful indicated that this was also the way they felt about thisplace.) I very much hope that each of you will be able to visit this sparse, pristine, rugged and eternally beautiful part of the world. Lt. Miller had his binoculars out looking for walrus on the shoreline this morning. There were none to be seen today. Maybe tomorrow?!

Question of the day: When are you guys going to send an e-mail!!!! (Very Big Grin!)

April 20, 2005March 18, 2021

Jim Jenkins, April 20, 2005

NOAA Teacher at Sea
Jim Jenkins
Onboard NOAA Ship Miller Freeman
April 18 – 30, 2005

Mission: Pollock Survey
Geographical Area: Bering Sea
Date: April 20, 2005

Weather Data

Science and Technology Log

You might want to begin by comparing yesterday’s barometric pressure (1002.8 millibars) to today’s pressure (1011.1 millibars). Knowing that a rising barometric pressure is an indication of good weather would give you an idea of the weather that we are enjoying right now. It is bright, sunny and warm for this part of the world. Last night, there was another indication that the weather today would be nice when I looked out the porthole to see a lot of pink in the sky just before I went to bed. Do you remember the saying, “Red sky at night, sailors delight?” Do you think this applies also to reddish shades of pink?

Sarah Thornton sits beside the instrument used to measure nitrate levels in the ocean. (The cylindrical device in the lower right of the photo.)

Tomorrow, the phrase, “Red sky in the morning, sailors take warning,” may apply! Matt Faber, Ordinary Fisherman, on the Miller Freeman is sitting across from me reading the paper as I type. Matt advises that we are expecting a drop in the barometric pressure tomorrow of about 10 millibars to around 1000.00 millibars. What do you think this means about tomorrow’s weather? If you predict that the weather will change dramatically you are correct. In fact, Matt notes that we are expecting high winds tomorrow. Winds are projected to come from the east at 35 knots per hour. Sea wave height will probably be 6 to 8 feet high. This is quite a change from today’s one-foot sea wave height, isn’t it?

I asked Matt about his experiences in rough weather at sea. He told me of a trip in February of this year when the sea wave height was in the 20-30 foot range. (This would make some waves higher than Mountain View School Elementary School!) Matt advises that the best strategy for these conditions is to “hang on,” and “put up a rail on your bed so that you do not fall out of bed at night.” I am taking his advice on these things as well as his advice to visit the ship’s doctor to get some medicine to prevent seasickness!

This is the operations officer Lt Miller. He knows a lot about marine geology. What are your questions about rocks, earthquakes, volcanoes, faults, trenches, tsunamis......? — This is the operations officer Lt Miller. He knows a lot about marine geology. What are your questions about rocks, earthquakes, volcanoes, faults, trenches, tsunamis……?

Visiting the bridge to get the data needed to start my journals to you is becoming a great opportunity. Do you remember the story of seeing a killer whale on my first trip to the bridge to collect data? Well, today I got another surprise! The operations officer, Lt. Mark Miller, called me over to look at a volcano that was spewing smoke. The view through the binoculars was stupendous! Unfortunately, the distance and the conditions did not make it possible to get a good photograph. By the way, the name of the volcano is Shishalden. It is on Unimak Island. This may be a great topic for research for some of you. I am looking forward to having the time to research this myself when I return home.

Today, I have talked with Sarah Thornton, a scientist from the University of Alaska Fairbanks. Sarah is here to deploy an instrument that measures the nutrients in seawater that feed all ocean life. In the past, sampling involved traveling to a location, taking a water sample, and then taking it back to the lab for analysis. Sarah’s instrument collects the data as it sits beneath the surface of the ocean. Sarah will come back in 6 months from the time she drops it off to pick it up. The instrument will then have 6 months of data which will be available to lots of people studying food chains in the sea.

This is the library where most of the logs to you are typed. The computer is put away right now so that it does not fall off the table with rolls of the ship. I am writing from "Data Plot" where computers are bolted down. — This is the library where most of the logs to you are typed. The computer is put away so that it does not fall with rolls of the ship. I am writing from “Data Plot” where computers are bolted down.

Sarah’s instrument will be placed below the large yellow doughnut centered mooring that I described on day one. ISUS is the name for Sarah’s instrument. The letters stand for In-Situ (Latin for “In Place) Spectrophotometric Underwater Sensor. The words are complicated, but the idea is not as complicated. Put simply, an ultraviolet light is sent through sea water. Different substances in the water absorb light at very specific frequencies. Nitrate, the primary food for phytoplankton, also absorbs light at a very specific wavelength. This enables data on nitrate level to be recorded. As noted earlier, Sarah will be able to take six months of nitrate level testing back to labs for analysis when she comes back to pick up her instrument next September or October. Scientists can then look at the nitrate levels to see how well fish populations will be fed in the future. Good nitrate levels mean that the fish will be well fed and plentiful. Lower nitrate levels may mean problems for fish and for fishermen.

I assumed that ISUS would be placed close to the surface where the sun’s rays were able to penetrate to start photosynthesis. I was a little surprised to learn that the instruments are typically placed at a depth of only thirteen meters. Can you think of a reason for this depth? If you guessed that they placed at this depth to avoid problems with ice, boat traffic and weather, you are exactly right.

Light penetration in the Bering Sea may be common at 40 meter depths under some conditions. Sediment in the water or a lot of phytoplankton in the water may lessen light penetration, however. And there is measurable amount of light at 100 meters in some parts of the Bering Sea. Do you think the 13 meter depth of the instrument is logical in light of all you know?

Personal Log

I am going to send a photo of my stateroom today. It occurs to me that you might find this interesting. The room is about 12 feet X 12 feet. It is divided diagonally into two smaller rooms. Each room has a bunk bed and two lockers. A shower and bathroom are in one corner of the room. I am lucky to have a good roommate.

Later today, I am going to go down to the gymnasium for a run. I have had little physical exercise since I got on the ship. I do not want to come home and have you guys run circles around me on our Tuesday runs.

Remember to let me know what you want to learn about, while I am on the ship. This is a great opportunity for you to impact your own education. Please take advantage of this. Question for the day: A major tsunami, or seismic wave, hit the coast of the United States more that forty years ago. Can you find the exact year and place?

April 19, 2005March 18, 2021

Jim Jenkins, April 19, 2005

NOAA Teacher at Sea
Jim Jenkins
Onboard NOAA Ship Miller Freeman
April 18 – 30, 2005

Mission: Pollock Survey
Geographical Area: Bering Sea
Date: April 19, 2005

Mr. Jenkins holding a temperature sensor.

Weather Data

Latitude: 55, 36, 50 North
Longitude: 155, 51, 00 West
Visibility: 10 Nautical Miles
Wind Direction: 164
Wind Speed: 18 Knots
Sea Wave Height: 1-2 Feet
Sea Swell Height: 2-3 Feet
Sea Water Temperature: 5 Degrees C
Sea Level Pressure: 1002.8
Cloud Cover: Cloudy

Science and Technology Log

The better part of the morning was spent putting temperature and pressure sensors in metal cages. I will send a photo with the subject line, “Metal Cages” so that you will have a good idea of the construction of these devices. The sensors mounted in metal cages are suspended from moorings at 3 feet intervals to give scientists a good indication of the temperatures at various depths in the ocean. Data collected from similar sensors has been collected for a long time and will continue to be collected well into the future. Scientists can look at the data collected over the years to draw conclusions about the patterns noted. For example, should temperatures continue to rise over the years, scientists might look for a reason for this rise in temperature. You have heard of the idea of “Global Warming.” Data collected in this project can be used to monitor the severity of this problem.

Today has been mainly a day of transit, the term used by NOAA folks to refer to travel to a work location. The down time gave me the opportunity to interview my roommate, Chris Garsha, an engineer with the Scripps Institution of Oceanography in San Diego, California. Chris and Lisa Munger, a doctoral student from the University of California at San Diego, are here to place instruments in the sea which will monitor whale calls. Chris and Lisa are great people. They provided a lot of good information which I will share with you now. Also, they volunteered to e-mail you with more information about whales when they return home to California. I gave them my card so that they would have your school address. First, I will give you the address of a web site that both Chris and Lisa recommended.

The site has sounds of whales which have been recorded by the instruments that Chris and Lisa are here to deploy. I know that you will enjoy this.

Do you remember studying sound waves in class? I think that you will remember that a wavelength is measured from crest to crest, or from trough to trough. Chris and Lisa use this idea when recording sounds of whales. They measure the frequency of whale sounds in Hertz (Hz). 1 Hertz (Hz) would be 1 wavelength per second. 40 Hz would be 40 wavelengths per second. 1 Kilohertz (kHz) would be 1,000 wavelengths per second. 40 kHz would be 40,000 cycles, or wavelengths per second. I hope that I have explained this clearly, please let me know if this is not the case.

Chris and Lisa are going to put an instrument in the water which will be attached the top to a huge yellow ball which will float just beneath the surface of the sea. The bottom of their instrument will be attached to one of the railway wheels we mentioned yesterday so that it will be in the same place when they come back to pick up their instrument in 6 months.

The instrument that Chris and Lisa are going to put into the sea has three tubes. One of the tubes is for power. The power is provided by the same D cell batteries that you use in your flashlight at home. Only in this case, the power is provided by 192 batteries!!!

A second tube contains a data logger to record whale sounds and associated electronics. This tube contains sixteen 80-gigabyte discs. This represents the computing power of sixteen lap top computers.

The third tube contains a hydrophone. This is a device that initially picks up the pressure caused in the water by whale’s sound. The pressure of the sound causes oil inside the hydrophone to move. This movement or pressure is picked up by electronics inside the tube and recorded.

As I noted earlier, Chris and Lisa are coming back in 6 months to pick up their instrument and analyze the sounds. Some of the sounds will be converted to spectrograms so that they can analyze the sounds visually. Loud sounds will show up on the computer screen in shades of red. Softer sounds will show in shades of blue.

Human hearing is in the 20 Hz to 20,000 Hz range. This will give meaning to some of the things I am about to tell you. For example, Baleen whales (Right Whales or Fin Whales) make lower frequency sounds in the 10 Hz to 10 kHz range. Would you be able to hear a Fin Whale making a sound at its lowest frequency? I look forward to your answer to this question.

Toothed whales (Dolphins, Porpoises, Killer Whales, Sperm Whales and Beaked Whales) make sounds at higher frequencies. This helps Chris and Lisa to tell a toothed whale from a baleen whale just by listening to their sound.

Did you know some whales make different sounds for different reasons? For example, a Killer Whale whistles at a lower frequency for social reasons of communication. Higher frequency clicks are used for echolocation, just like the Little Brown Bats which live in caves there in Virginia.

Chris and Lisa are scheduled to put their instrument into the water shortly. Please let me know if you would like an update on its deployment?

Personal Log

Your teacher had an old man’s day, retiring at noon for a two-hour nap. Some seasickness had persisted so I decided to see it I could sleep it off. Well it worked! After not eating all day, I had a delicious dinner that ended with my all time comfort food, banana cream pie. I feel great!

I must confess that a dose of Dramamine taken just after getting up may have helped the situation. You may find humor in the fact that I chose the Less Drowsy Formula because I did not want to waste time sleeping while I was here!

Question for the day

Today’s seawater temperature is 5 degrees Celsius. Can you convert this to degrees Fahrenheit?

April 18, 2005March 18, 2021

Jim Jenkins, April 18, 2005

NOAA Teacher at Sea
Jim Jenkins
Onboard NOAA Ship Miller Freeman
April 18 – 30, 2005

Mission: Pollock Survey
Geographical Area: Bering Sea
Date: April 18, 2005

Mr. Jenkins with NOAA Ship MILLER FREEMAN in the background.

Weather Data

Science and Technology Log

I arrived in Kodiak on the afternoon of April 15. The first few days in Kodiak were spent helping scientists and deck hands load equipment and assemble moorings. The sensors are used to gather information about currents, salinity (saltiness), water temperature, weather, and ocean organism populations. Some of the moorings are so large that a crane needed to move them about the deck for assembly.

One of these moorings will ride on the surface of the ocean on a doughnut shaped center about the size of a monster truck tire. A 12-foot high triangular tower made of metal is attached to the top of doughnut like piece with bolts. This part of the mooring collects weather data. A second triangular metal tower is bolted to the bottom of the center piece. This section is made of different types of metal which enables collection of data on salinity. Three 110-pound metal triangles attached in the center of this section hold the mooring down in the water. The whole apparatus is anchored to the bottom of the ocean using old railway wheels. What do you think of this form of recycling? I am sending photos of the mooring as well as the wheels used to anchor the mooring. Please take a careful look at the photos. I know that you will have excellent questions as usual. Be certain that I will post replies to your questions quickly.

Above is the mooring. Ms. Thornton’s instrument to determine nitrate level will be placed beneath this.

Most of this cruise will be involved with the study of conditions above a relatively shallow shelf in the Bering Sea. Water depths in this section of the sea are less than 100 meters. Your knowledge of the food chain will enable you to see that study of this productive zone is not an accident. The relative shallowness of the water enables the sun’s rays to penetrate to provide food for plant plankton or, phytoplankton, which make their food by photosynthesis. Animal plankton, or zooplankton, eat the phytoplankton starting the food chain which provides nutrition for all ocean organisms as well as you and me!

Walleye Pollock are the most harvested fish in the Bering Sea. Each year, about 1,000,000 metric tons of this fish are caught and sent to food processing factories. Can you tell me how many pounds make up a metric ton? This may require a little research as well as your math skills, but I am sure that you can do this. I look forward to your answer.

You may have eaten Walleye Pollok and not known it! Much of the fish caught is processed into fish filets or fish sticks. You probably have eaten Walleye Pollock if you have had a fish sandwich at a restaurant. Some of the walleye harvest is made into a paste. This paste is added to crab products in the artificial crab that you may have enjoyed. Does this make you want to look at food packages and do other research regarding the source of your food? Anyway, I hope you have enjoyed your taste of the bounty of the Bering Sea!

I needed to go up to the bridge yesterday to get the data which begins this journal. A Killer Whale came to the surface right in front of the ship while I was recording the data. Awesome!

Personal Log

Kodiak was one of the most beautiful places I have ever visited. I particularly enjoyed hikes along the beaches, through the spruce forests and on the hillsides. A box of rocks was put into the mail to all of you on Saturday. The rocks came from a gorgeous cobble beach called Mayflower Beach. I think you will enjoy the way the sea smoothed your rock to leave the wonderfully sculpted pieces which you will soon have. I hope you enjoy these treasures of nature!

A sculpin was one of the fish caught on a fishing trip yesterday. I remember how interested all of you were in the report on sculpin done by Alison. A photo was taken before releasing the fish. I am sending a copy of the photo.

I have proven that it is possible for a human being to become seasick on a 215 boat in 4-foot seas (Very Big Grin)! Anyway, I am peachy now and look forward to your replies. I miss you guys!