Wednesday, 12 January 2000: 2:30 PM
Using an ocean general circulation model, we analyzed features of
ocean responses to the major differnces among
surface wind fields derived from the NASA Scatterometer (NSCAT),
Special Sensor Microwave/Imager (SSM/I), and operational numerical
weather prediction model of the European Center for Medium-Range
Weather Forecasts (ECMWF) for the NSCAT period from September 1996 to June 1997.
In the tropical Pacific, the strongest
bias for thses surface wind data is in the equatorial eastern Pacific
for both wind direction and speed. Significant differences also exist
in the north eastern Pacific.
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