Category Archives: Bering Sea Expedition

Sunday on the Healy

It was a foggy snowy day on the Healy yesterday as we steamed north towards St. Lawrence Island and the northernmost section of our cruise.  In Sunday tradition on the Healy, lunch was a barbeque on the helo deck.  The big grill was pulled out on deck and the rest of the food was served in the hangar.  It was pretty neat to be having a barbeque in the middle of the Bering Sea surrounded by ice as we were cruising along.  

We are in pretty heavy ice now and the one thing that strikes me is how fast the Healy can move through the ice.  We were steaming at 13 knots yesterday and blasting through ice like it was nothing.  The views from the bridge were beautiful despite the lack of visibility.  The sea of white melted into the white sky with seals dotting the ice from time to time.  It was a very nice Sunday.

 

  

 

April 26- Owls in the Bering Sea?

In the fog, we were steaming to our next station in the morning.  We are in the southern part of our cruise again so we are out of the ice, but we are heading north so we should be back in the ice shortly.  One of the first orders of the day was to collect the sediment traps that had been deployed yesterday.  The scientists deploy the sampling device for 24 hours at which time it floats along in the currents until it is retrieved the following day.  (More to come on this.)  The seas cooperated and were very calm for a successful retrieval.  

A little while later, I received a page from the bridge telling me that there was an owl flying around the bridge.  AN OWL?  I went up to the bridge and I had missed the owl.  I was reassured that he would come back because owls don’t belong in the Bering Sea and he would want to come back to the shelter of the ship.  A few minutes later, he flew back into view and we had a great look at him.  He looked very tired so we hoped that he would land on the ship to rest.  Indeed he did, landing first on a small railing, then on the A-frame, and finally on the bow where he hung out for a while.  The bird researchers determined that it was a short-eared owl.  This little guy was far from home but it was very cool to see him.  Definitely the highlight of the day.

  

 

Studying the Bugs of the Ocean, the Copepod Team

Out in the cold and dark early morning the zooplankton ecologists wait for a net tow to come up from the depths in order to collect krill and copepods for their experiments.  Once the net comes up, they put the “bugs” into coolers and get ready to go into the cold room to sort them.  The cooler is teeming with krill, copepods, Clione (a type of pteropod), amphipods and other varieties of critters.  I follow them into the cold room where they divide the plankton and begin sorting through to get the dominant species to run their grazing and other experiments.  Dr. Carin Ashjian from the Woods Hole Oceanographic Institution and Dr. Bob Campbell from the University of Rhode Island, with the help of Phil Alatalo and Donna Van Keuren, lead the team which is conducting experiments about the grazing impacts of the mesozooplankton and the fecundity of the animals.  

“Deploying the ring net used to collect the copepods and krill needed for the team’s experiments”

 

Their first set of experiments focuses on the grazing of the dominant species of the mesozooplankton, particularly copepods and krill.  The mesozooplankton plays a key role in nutrient cycling in the ocean as they provide a key link between the primary producers (phytoplankton) and the larger animals.  Their waste settles to the sea floor providing key nutrients for the benthic system.  They sort the animals and place individual species into jars with seawater collected from the depth where the animals live.  The water is tested for the beginning concentration of chlorophyll which indicates how much food is in the water at the beginning of the experiment. Most mesozooplankton are omnivorous but the team uses chlorophyll to estimate how much of the plant biomass is eaten and to determine the proportion of primary production consumed by mesozooplankton.  The jars are then placed in various wraps to emulate the light conditions they would have at depth and they are placed in an incubator of ambient seawater for 24 hours where they rotate and mix constantly.  After this period, the jars are brought to the cold room which is kept at -1 to -1.5 degrees Celsius, where the animals are removed and put into dishes and the water is divided into various bottles for analysis.  The water will then be tested for chlorophyll concentration to quantify the changes to biomass.  The animals are then dried and packed away to be analyzed for carbon content once back on land along with samples of microzooplankton, phytoplankton and ice algae to determine the food preferences of the bugs.  In this way, Dr. Ashjian, Dr. Campbell, et al are able to quantify the role the mesozooplankton plays in the trophic structure (food web).  

“Phil Alatalo sorts through the sample for animals to use in the experiments”

 

“Copepods”

“Krill”

“On the bow, the incubators hold the samples for 24 hours in ambient sea water with constant agitation”

 

Their second experiment is looking at fecundity in females, counting the number of females with eggs, counting eggs and measuring rates of hatching.  The females are collected and put into the  “bug hotel” which I am told has a total occupancy of 120 copepods and is located in the cold room where they check in for 24 hours at which time their eggs are counted and a sub-sample is taken for the hatching studies.  These studies seeks to determine the timing and magnitude of reproduction in relation to what the copepods are eating, is it a function of lipid (fat) reserves, the presence of ice algae or other algal species?  These studies can then give the scientists an index of individual growth and food limitations on this growth.  

“Dr. Campbell carefully picks female copepods out of a sample to put into the bug hotel for their egg studies”

 

“Dr. Campbell puts a tray of female copepods into the bug hotel for the egg growth experiment”

 

The copepod team provides key information to the understanding of a key element of the ecosystem.  By sampling in different areas from north to south in the Bering Sea and at various depths and ice coverage, the team is analyzing the effects of the seasonal ice and what could happen if it is not here. Where will the carbon go if the sea warms and there is less ice, to the mesozooplankton or to the benthos (sea floor)?  

 

“Dr.Ashjian and Dr. Campbell remove the animals from the experiment jars in order to preserve them for analysis of carbon in the lab. The water is siphoned out for chlorophyll concentration studies.”

 

April 25

Today has been a slower day.  The sun is shining and the sea is calm.  It was a beautiful morning with temperatures around freezing here in the open water.  We are heading towards the shelf edge to do some benthic sampling before heading back to our process station to assess any changes on our quest to find productivity and a possible phytoplankton bloom near the ice edge.  It is a relatively quiet day on the ship with some samples being processed and others collected.  Birds were hanging around the ship as we were on station with the multi-core in the water.  We are in 500m of water so the sampling took a fair amount of time.  

I took this opportunity to sit outside and look out at the Bering Sea and think about how beautiful and calm it is out here today and how quickly the weather out here can change.  However, the weather maps indicate that a high pressure system is coming through so hopefully that means nice weather for the next few days.

As the day continued, the clouds took over the sunny sky and the sky became dreary.  The seas remained calm.  We are doing a zigzag pattern for our stations now and came into a productive area in deeper water.  

I stayed up to see the net tows which happened around 1am.  I was anxious to see what kind of critters were in the water.  There were three net tows at this station and sure enough, there were lots critters in the water: copepods, krill, pteropods, polychaete worms and some little fish, among other critters too small to identify.  The water is mostly filled with copepods which are small crustaceans.  We are now headed north to our next station and tomorrow I will find out where we are going next.  We should be back in the ice by Sunday so I am looking forward to that! 

“The Fan Tail”

 

“The krill sampling team and the marine science technicians bring in the bongo nets in the darkness” 

 

“A bucket teeming with copepods, krill and other plankton. Without a microscope, it looks like thick red/orange soup.

 

 

 

Scientist Profile: Dr. Carin Ashjian, Chief Scientist

 

Yesterday, I had a chance to sit down with the chief scientist, Dr. Carin Ashjian, a zooplankton ecologist from the Woods Hole Oceanographic Institution, to find out more about the mission of the cruise, her role as chief scientist of the expedition and her research.  

The mission of the cruise is to determine the importance of the ice and the seasonal melt on the ecosystem in order to determine how different ice conditions affect it.  Essentially, the scientists want to know how important the ice is and what would be the impact if the ice disappeared in the future.  On this cruise, the researchers are looking mostly at the base of the food chain, the phytoplankton, zooplankton, sea floor gas exchange and animals and some physical oceanography to put it all into context.  

With twelve projects going on and forty-six scientists on board, there is a lot to manage and Dr. Ashjian must make sure that everyone gets the samples they need to complete their projects.  This is quite a challenge!  Many of the projects are time dependent or location specific so a careful plan is key.  Unlike in the laboratory, variables change at sea, so while a cruise plan may seem perfect while on land in the planning stages, sea conditions, weather and in the Bering Sea, the ice, may force the original plan to be changed.  Improvisation and flexibility is the key but any changes must be made within the parameters of the project.  For example, one team is studying krill and their samples must be collected at night.  For this reason, we must be at the sampling location around 3am or the work cannot be completed in the dark.  (The sun has been setting at 11:30pm and the days are getting longer and longer.)  Much of the work is collaborative so the samples must be taken at the same location.  For this reason, most of the sampling is completed in the middle of the night.  Dr. Ashjian is responsible for discussing the cruise plan with the Captain, officers and crew and making sure that everything runs smoothly.  

In addition to the multitude of responsibilities associated with being chief scientist, Dr. Ashjian is conducting her own research on copepods and other dominant mesozooplankton (highlights coming soon).  She adds that this is one of the most challenging jobs she has had.  Thus far, all of the scientists are learning a great deal and collecting samples to analyze when back in the lab.  

Our next course of action is to look for areas of high production near the ice edge and continue sampling before heading north to do a specific transect in the ice on Sunday. 

 

 

 

April 24: Ice and Sun

I started the day photographing some net tows in anticipation of learning about the mesozooplankton (copepods, krill, etc) grazing experiments being conducted by a team of scientists on the ship.  I stayed out on deck for quite a while to observe, as various plankton was being collected along with some bottom grabs of mud.  It was quite chilly at about 25 degrees Fahrenheit with a stiff breeze.  The swells were sizable but not too bad.  The water temperature was hovering around -1.7 degrees Celsius, just above the freezing point, which is lower than the freezing point of freshwater.  

Shortly after we headed back north and were in the ice!  I was sitting at my desk and started hearing the crunch of the hull breaking through the ice at which point I looked at the images available from the bridge and saw that indeed we were surrounded by large islands of ice intermixed with slush.  It looked beautiful and endless so I headed outside to see it for myself.  (My desk area is in a lab without any portholes so it is easy to lose track of what is going on around me.)  The sun had come out and it was shining on the endless white undulating sea.  I headed up to the bridge to get a better vantage point at which time someone spotted some seals on a ice patch.  They were in the distance but it was still nice to see a seal or two.  Hopefully it is only the beginning of the beautiful things that are to come.  We remained in the ice for a little while and then just after dinner we were back in open water.  There is something amazing about crossing the ice edge.  The swells roll in seeming to go under the ice and the wake of the ship pushes the ice aside with ease.  

Now it is about 10:00 pm and it is still sunny with some clouds.  The sun sets at 11:30pm so I am hoping to see a beautiful Bering Sea sunset.  It has been cloudy every other evening that I have been out here so I am anxious to see a setting sun.  

 

April 23: ICE!!!

As we made our way through water sampling stations, we all anticipated the approaching ice edge.  We were heading north so it was just a matter of time and we all hoped that we would come to it during the day.  The day was cold and started out calm and cloudy but by midday the sun was shining although it was still quite chilly and the wind began to pick up.  There were gulls and other small birds around the ship as we cruised north at 15 knots.  The water temperature was dropping indicating that we were getting close to the ice.  

Shortly after dinner, the bridge made an announcement over the pipes (loudspeaker) that the Healy would be in ice in ten minutes.  I quickly gathered up my cameras and headed out on deck and up to the bridge to see the approaching ice edge.  It was beautiful with the sun shining.  Large and small pieces of ice bobbed in the water.  The ship cruised right through and it was quite beautiful.  We did some sampling and then turned south and out of the ice to follow our research transect.  We should return to the ice sometime tomorrow.  Hopefully the sun will still be shining and we will get into thicker ice.  

 

The Multi-Core Team – Studying the Dynamics of the Sea Floor

I have spent the past two days learning about the multi-core, a state of the art benthic (sea floor) sampling device.  The multi-core is unique in its ability to preserve the sediment water interface while sampling.  This is a critical zone for the exchange solutes between the bottom and the water.  Nutrients, dissolved gases, and other elements collect in the bottom sediments and their interaction with the water above is one important element of the research being conducted by the researchers on this cruise. 

Paul Walczak, the coring guru, prepares the multi-core for deployment. 
 

Dr. David Shull from Western Washington University and Dr. Al Devol from the University of Washington lead the team along with their graduate students Emily Davenport and Heather Whitney.  They are studying how the sea ice and its melting are affecting the processes on the sea floor, specifically where the organic matter accumulates and the effects that the burrowing animals, such as tube worms and clams, have on the nutrient supply to the overlying water.  They use the multi-core instrument to collect their samples which they then analyze to get profiles of nutrients within the layers of the sediment.  They measure nitrate, nitrite, ammonium and nitrogen gas, key components of the nitrogen cycle, to learn about the nitrogen levels in the sediment along with oxygen, silicate, phosphate and radon which Dr. Shull refers to as the “magic gas.” 

By collecting the information about the gases and nutrients, the researchers hope to unravel the mystery of how the ice melt and presence of more organic matter in the water column affects what is on the sea floor.  Will a larger food supply from increased ice melt and the following increase in mud-dwelling organisms increase or decrease the amount of nitrogen in the water just about the sea floor?  These are the big questions that this group of scientists are trying to answer.  

Why is this important?  The Bering Sea has a remarkably productive benthic system. From clams and tubeworms to King Crab and Pollock, the exchange of nutrients from the bottom to the waters above is a key component to the food web.  It is important to understand what are the limiting nutrients in the Bering Sea and how they affect ecosystem structure.  Looking at what is in the water column and what ends up on the bottom and how it interacts with the sediments and its eventual return to the water column is of vital importance to our understanding of exactly what is happening here.  In our world of climate change, the effects that more or less ice will have on the system is of vital importance to gaining insight into what the consequences of changes in the ice will have on the entire system in the future. 
   

Bringing the multi-core back on board after collecting sediment cores at 3500 meters below. The winch and A-frame do most of the work but the crew on deck must guide it in gently to not disturb the samples or damage the instrument.
 

The multi-core can take up to eight samples each deployment.  A good sample has clear water on top of the sediment and the interface between the sediment and the water should be undisturbed.

 

Dave Shull examines a core.  This is a good sample as the water above the sediment is clear.
 

Heather Whitney takes samples from the core to process later.  The core is carefully sliced in order to sample the various layers of the sediment.
 

Emily Davenport gets ready to extrude the core from the sampling container in order to begin sampling. 
 

A core is sampled for oxygen using a specialized probe that records data and gives a profile of oxygen concentration in the core. 

 

April 22- Sediment Traps and Science Meeting

We are still in open water working at a deep station.  The weather is beautiful with calm seas and bright sunshine.  Yesterday some of the scientists deployed a floating sediment trap that drifts in the sea for about 24 hours until they go and retrieve it.  After completing the multi-cores, we head off to find and recover the sediment trap.  This involves a small boat being launched over the side and an elaborate plan to get the instrument back on deck with samples intact.  The weather was on our side for this retrieval and it went off without a hitch.  However, I would not have wanted to be in the small boat which was getting tossed around in the big seas.  

“Retrieving the Sediment Trap”

The evening continued to be beautiful with flocks of gulls and other small birds flying around the ship. Then it was time for the science meeting to determine where and what we were going to do next.  

All of the scientists convened in the science lounge to discuss the plan.  Most of the transect work and time specific samples had already been collected and we had a few days to work with before we needed to head up to our next definite sample site so the question of what all of the scientists wanted to do was the topic of the meeting.  Carin Ashjian, the chief scientist, began by going over what we had accomplished on the cruise in the past few days and then outlined the options for the next few days.  After compiling the input of all of the principal investigators, it was decided to look for an area of production where there could be a lot of phytoplankton and then head north to look for the ice edge.  

We should get into the ice sometime tomorrow evening so I am very excited as it has been a few years since I have been in a frozen ocean.  

 

Listen and Watch Some Science on May 1

One of the scientists on board is conducting a “webinar” on May 1 at 2:45 EDT for anyone who is interested in hearing and seeing more about the science being conducted on the cruise.  Here is some more of the information about the event.  Emily Davenport, a member of the Multi-core team, is coordinating it.  Hopefully all can join in to learn about the great science.
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Participate in Live from IPY events! 
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Join us for a real-time, Internet “webinar” on 1 May 2008 with Emily Davenport and the research team in the Bering Sea.

Event starts at 10:45AM Alaska Daylight Time [8:45AM HDT, 11:45AM PDT, 12:45PM MDT, 1:45PM CDT, 2:45PM EDT]. The event will last about 1 hour and participants will get a chance to hear about the research being conducted as well as interact with researchers and Emily Davenport.

These events are FREE to join.  For more information and to register for this “Live from IPY” event, go to: http://www.polartrec.com/live-from-ipy/registration

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