Jillian Worssam, July 10, 2004

NOAA Teacher at Sea
Jillian Worssam
Aboard NOAA Ship Miller Freeman
July 5 – August 1, 2004

Day: Five
Saturday July 10th, 2004 1:20

Longitude: 59° 50 Sea Wave Height: 1-2′
Latitude: 173° 14 Swell Wave Height: 0′

Visibility: 2.1miles fog Sea Water Temperature: 9.4C
Wind Direction: 121.6 Barometric Pressure: 1019 high pressure
Wind Speed: 11.3 kts Cloud Cover: complete 100%

Haul Data – Methot
Depth of haul: 20 meters
Temperature at depth: 7° C approximate
Species breakdown: walleye pollock year 0, Amphipod- type of crustacean, Chrysora jellyfish

Science and Technology Log:

The Methot haul is when the nets are set out, but at the end there is a cylindrical tube of PVC. It is this tube in which the sample will be taken. Holes are drilled in the side to let the water run through, but there is a mesh screen which prevents the specimens from escape. The purpose of the Methot trawl is to collect younger samples of fish, and as the younger pollock tend to stay higher in the water, and this device is perfect for sampling. Most of the pollock were year zero meaning that they spawned this past April. There is also a relationship between the juvenile pollock and the jellyfish as the Jellies (common term) provide shelter for the young fish. Walleye pollock are cannibalistic and will eat younger smaller fish that could well be their own children.

One of the scientists on board Taina Honkalehton has just returned from Tasmania where she was contracted by the Australian government to study orange roughy, a species that has been over harvested that they are now trying to save as a viable harvest species. Pollock on the other had is a well managed species, where at this time approximately 20% of the population is being utilized for commercial ventures. Pollock are the fish of fish sticks, a very important economic product on a global scale, with pollock as the largest single species fishery in the world making oceanic ecosystem management very important. Approximately 1.8 million tons of Pollock are harvested annually. Part of the management plan for pollock is based in part to their relationship to the stellar sea lion. As an endangered species management needs to look at fish harvesting and see if there is a relationship between the decline of the sea lion and changes in fish numbers.

Personal Log:

Running late tonight, having too much fun gutting fish, measuring jelly fish and cleaning. I have often wondered the purpose of jelly fish. As an Easterner by birth my only experience has been the Portuguese Man of War, the stinging variety that invariably closed our local beach. The jellyfish we have been seeing not only provide habitat for many other aquatic species, but that are also a nutritious food source. Monterey Bay Aquarium has a wonderful display of jelly fish. An amazing species, so beautiful in their basic simplicity.

I promised I would talk about the spinner, which no one has been able to give me a scientific designation for. This amazing piece of technology is a circular window approximately two feet in diameter, the ships windshield. During winter months the entire window of the bridge often freezes up, and this device, through the use of centrifugal motion, manages to keep an area clear for viewing. The glass of the spinner, you guessed it, spins at a very fast rate thus keeping the viewing surface clear.  It is a funky tool, and so far my favorite on the bridge.

Dr. Laura Brezinsky, April 18, 2004

NOAA Teacher at Sea
Laura Brezinsky
Aboard NOAA Ship Miller Freeman
April 8 – April 22, 2004

Day 8: Sunday, April 18, 2004

Latitude: 52.28.03N
Longitude: 171 10.7

Weather: continuous clear
Visibility: 29.5-49.5 ft (Very High)
Wind direction: 285 degrees
Wind speed: 35 (m/s)
Sea wave height :up to 16 feet
Sea water temperature: 4.1 Degrees
Sea level pressure: 1007.5

Science and Technology Log

The above data is from 0800 this morning. Last night the weather came up but we continued out to Amukta pass to try and recover 4 buoys. Unfortunately the waves and wind were too big for operations. This morning we are hiding on the lee of a small Aleutian island tucked in between 3 volcanoes (see attached photo) waiting to see if the weather subsides. We are scheduled to arrive in Dutch Harbor on April 21 or 22 so we can wait here for a couple days in the hopes we can grab those buoys because that is our priority at this point. So, no CTD’s were done and no buoys recovered

Personal Log

Right before bed last night I made my nightly visit up to the bridge. The waves were pretty big and it was fun riding them way up high on the bridge with the knowledge that this boat has been in much worse conditions during is decades of service. After I left the bridge the captain did report seeing “green” water which happens when the waves get so big that they hit the windshield of the bridge so far down from the peak that you see green water.

OLYMPUS DIGITAL CAMERA

Laura

Dr. Laura Brezinsky, April 17, 2004

NOAA Teacher at Sea
Laura Brezinsky
Aboard NOAA Ship Miller Freeman
April 8 – April 22, 2004

Day 9: Saturday, April 17, 2004

Latitude: 54.58.615
Longitude: 162.27.117

Weather: continuous clouds with drizzle
Visibility: 29.5-49.5 ft (Very High)
Wind direction: 181ees
Wind speed: 30m/s
Sea wave height: up to 20 feet
Sea level pressure: 996

Science and Technology Log

Last night we spent the entire night steaming south west down the Aleutian island chain, through the Unimak pass to the western side of the islands and past Dutch Harbor. Tonight we plan on picking up 4 moorings at Amukta pass and no new buoys will be deployed. The decision to move to the west side of the chain was made due to a small storm with 5 knot winds on the east side of the chain. If the weather improves we will move back over to the east side of the chain in a day or 2.

Personal Log

Last night I was awoken at 2:00 AM by some large waves that were tossing the boat (and me) back and forth. I kept thinking…”this boat has no centerboard” and “should I wake

up my roommate?” In the morning I discovered that my roommate was already awake and…this boat can take a lot more than what we saw last night. All of the tests are done with the centerboard up so we are still well within the limits of this boat. This journey has been an invaluable experience but I am very much looking forward to arriving in Dutch Harbor and seeing the wild horses that live there.

Question of the day: What are the factors that effect the formation of waves? How do the weather patterns differ between the Gulf of Alaska and the Bearing Sea

Laura

Dr. Laura Brezinsky, April 13, 2004

NOAA Teacher at Sea
Laura Brezinsky
Aboard NOAA Ship Miller Freeman
April 8 – April 22, 2004

Day 5: Tuesday, April 13, 2004

Latitude: 59.05.72N
Longitude: 151 00.14

Weather: continuous clouds
Wind direction: 60 degrees
Wind speed: 19m/s)
Sea wave height: less than 2 feet
Sea level pressure: 13mb
Cloud cover: Cumulus

Science and Technology Log

Yesterday we failed to retrieve the buoy that had lost its floaters but we did successfully deploy a new buoy. During the night the boat sailed south west to our present position off the coast of the southern end of the Kenai Peninsula. This morning we deployed another buoy and took CTD readings. We have one or2 more buoys to recover and deploy and they we will be picking up several buoys that will not be replaced because their projects have completed.

Personal Log

Last night at around midnight, the ship finally got an hour of down time and I got to fish. No one else was much interested so I was out there on the stern of the boat in the middle of the night watching the sea birds and hoping for a bite. I got to thinking about all the different types of birds out here and all their different strategies. Some stay here year round while others migrate to warmer waters and return.

Question of the day: What species of Plover migrates between Hawai`i and Alaska. Illustrate the migration patterns and summarize how those patterns have been elucidated.

Laura

Dr. Laura Brezinsky, April 12, 2004

NOAA Teacher at Sea
Laura Brezinsky
Aboard NOAA Ship Miller Freeman
April 8 – April 22, 2004

Day 4: Monday, April 12, 2004

Latitude: 59.31.830N
Longitude: 149 10.28’W

Weather: clear Visibility: 29.5-49.5 ft (very high)
Wind direction: 355 degrees
Wind speed: 6 (m/s)
Sea wave height: virtually flat
Sea level pressure: 143mb
Cloud cover: Nimbostratus

Science and Technology Log

This morning we are off the coast of Seward. We have been having difficulty retrieving a mooring because it is not vertical in the water. At the base of the mooring there is a switch that releases the mooring from the anchor by remote control. The switch also has a sensor that tells the ship what the position of the mooring is. Apparently the mooring is horizontal in the water rather than vertical and that is likely the reason why we cannot
find it. The boat will return with a remote rover that will find and retrieve the mooring.

For now, we will continue on and get the next mooring which is closer in to the coast.

Laura waiting for a mooring.
Laura waiting for a mooring.

Personal Log

The seas are flat, the sun is shining and the coast is stunningly beautiful. We are close enough to land that I can see individual features. There is a very large coastal glacier directly inshore from us. I will try and look up the name of that glacier and report tomorrow on that.

Question of the day: What is the definition of a glacier? How are glaciers being used to track global change over geologic time?

Laura