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Switchyard remote sensing



Mean DJMF ice motion of the switchyard 2003- 2004.


Anomalies of ice motion (vectors) and surface air pressure (contours), relative to 1978-2003 means.

Ice motion is OI blend
of buoys and passive
microwave.

 

Ice transport in the Switchyard
(here, across 45°W)

Anomalously eastward in the 1990’s

Anomaly is small recently, but westward in the Lincoln Sea

 
 
     
Polar Science Center
Applied Physics Laboratory
1013 NE 40th Street
Seattle, WA 98105
206-543-1300

University of Washington


This material is based upon work supported by the National Science Foundation under Grant No. 0230427.
Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the
National Science Foundation.

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