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 Dispatch 16 - September 25, 2003
 By C. A. Linder
 
 Weather conditions: Overcast skies, calm winds and seas,
              air temperature 28°F
 
 
 I don't think I have ever seen Bob Pickart happier. The WHOI mooring
            crew brought four more moorings safely on deck today, taking advantage
            of the ice-free, calm open water. To
            top it off, all of the instruments that we have downloaded data from
            so far were carrying a full load of 14 months of oceanographic data!
            There is always an element of risk with moorings. The ocean is a very
            hostile environment - moorings can become dislodged and drift away,
            they can fail to release, or the instruments can just simply not work.
            The entire science crew is ecstatic - data of this kind has never
            before been collected in the Arctic Ocean. What's so special about
            this mooring data? The spacing of the instruments, in the form of
            a picket fence
            across the shelfbreak, allows us to see a cross-section of the
            temperature, salinity, and currents of this part of the Beaufort Sea
            over the entire year. Sarah Zimmermann worked for 20 hours straight
            yesterday checking over the moored profiler CTD data. Dan Torres has
            been working nonstop today extracting the
            current data from the moored ADCPs.
            I asked Bob how long it would take to analyze all of this data. He
            replied: "at least five years."
 
 I have received several questions from Mrs. Werner's 6th grade
            class at the Morse Pond School.
 
 Question: How thick is some of the ice on this trip
            compared with last year?
 Answer: Last year the ice was dense, but broken into
            small chunks. This condition is known as "brash ice." Check
            out this photo
            of John Kemp and Dan Torres deploying a WHOI mooring last year. This
            year, we haven't seen a single chunk of ice since our CTD work in
            the northern Chukchi Sea. This is mostly a function of the time of
            year. Last year's deployment cruise on the Polar Star took
            place in July and August. At that point, the ice in the Chukchi Sea
            and southern Beaufort Sea was melting and breaking up, but hadn't
            completely melted away. This September, the annual ice has melted
            back as far as it will go... It's only a matter of time before new
            annual ice starts forming, since this process begins in October. The
            ice edge creeps back, slowly covering the Western Arctic with a layer
            of new annual ice. Earlier in the cruise, when we did see ice,
            it was similar to what we encountered last year - broken chunks floating
            in loose congregations. We have done very little ice breaking this
            year - mostly just "ice pushing!"
 
 Question: What has been the most interesting finding
            on this trip so far?
 Answer: WHOI Principal Investigator Bob Pickart is
            elated by the performance of his moored instruments. This quote helps
            put it in perspective: "We have just looked at the data from
            one of the coastal moored profilers. This one instrument performed
            four CTD casts per day for 14 months... That's 1,600 CTD casts! In
            comparison, here we are on the Healy on CTD cast number 121."
 
 This question comes from David, who's in 4th
            grade at the Mullen Hall School in Falmouth,
            Massachusetts.
 
 Question: If the wind was heading north through the
            eastern hemisphere over the north pole into the western hemiphere,
            once it passed the north pole would it be heading southwest? P.S.
            If you are standing on the north pole, how do you describe the direction
            of the wind?
 Answer: Hi David, good question! Winds are always
            named by the direction that they originate from. So, you would call
            that northbound wind a "southerly." As the wind crosses
            the pole, it automatically becomes a "northerly" since it
            is coming from the north. By that convention, if you're standing directly
            at the north pole, any wind you feel would be a "southerly"
            since the only direction you can go from the pole is south!
 
 
 
              Tonight the CTD watchstanders, led by CTD expert
            Marshall Swartz, will be testing the
            CTD sensors that will be redeployed on the moored profilers. Carin
            Ashjian will also do another net tow at 4AM, so we'll see if she finds
            some more copepods. Tomorrow we will recover the last two WHOI moorings
            and Lisa Munger's Acoustic Recording Package (ARP).
                |  |  |   | John Kemp climbs out of a storage hold deep in the bowels of the ship. |  
                | Click
                  to enlarge |  
 If you have a question about Arctic oceanography, shipboard life,
            or what we had for lunch on the Healy, send your question
            to arcticedge@whoi.edu. I'll
            do my best to find the answer and post it in a dispatch.
 
 
 
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