AIDJEX Bulletin #40 - Polar Science Center - University of Washington
AIDJEX Bulletin #40 - Polar Science Center - University of Washington
AIDJEX Bulletin #40 - Polar Science Center - University of Washington
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situation for operations. That period corresponds to the beginning <strong>of</strong> the<br />
<strong>AIDJEX</strong> experiment, when there were few data on barometric pressure and ice<br />
movement and the ice model used in that simulation did not accurately<br />
represent the yield strength <strong>of</strong> the ice. Our current work is compared<br />
with another simulation performed for the Outer Continental Shelf Environmental<br />
Assessment Program (OSCEAP), which simulated conditions in the<br />
nearshore Beaufort Sea during the winter <strong>of</strong> 1976. During that time there<br />
were accurate data on barometric pressure and buoy motions, and the model<br />
was modified to represent accurately behavior <strong>of</strong> the ice. It has been<br />
shown that this simulation is extremely accurate in representing the motions<br />
<strong>of</strong> the ice pack throughout the region <strong>of</strong> interest (Pritchard et al., 1977).<br />
In determining how the <strong>AIDJEX</strong> model may be used as a short-term ice<br />
forecasting tool, our specific tasks have been to determine (1) how the<br />
National Weather Service weather predictions are input best as driving<br />
forces and how much error is introduced by inaccuracies in the predictions;<br />
(2) what additional motions must be specified from data buoys to provide<br />
necessary boundary conditions and other data: and (3) how to interpret the<br />
velocity, ice state, and strain and stress states to provide necessary<br />
forecasting aid.<br />
The first task is addressed in detail in this report. The second has<br />
been addressed in part by Pritchard and Thomas (1977), who determined how<br />
the boundary velocity subject to random errors with zero mean affects solutions<br />
in the interior. The third is addressed partially by describing the<br />
results <strong>of</strong> the first two, but it also has been discussed separately by<br />
Coon et al. (1977), who describe another simulation and its application to<br />
prediction <strong>of</strong> ice conditions on the time and space scales <strong>of</strong> interest.<br />
This report is taken from an annual report to the NOAA Environmental<br />
ResearchLaboratories describing initialwork to determine how effective the<br />
<strong>AIDJEX</strong> model would be at short-term ice forecasting along the north slope<br />
<strong>of</strong> Alaska (Pritchard and Coon, 1977). It is reprinted here to make the<br />
results more available to the general scientific community.<br />
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