The study of mesoscale ocean windsSAR data gathered over the U.S. East Coast are used to infer near-surface wind speed, using a simplified model to relate the strength of the 30 to 40 cm SAR backscatter to surface wind speed. It is found that the SAR backscatter is nearly isotropic with a wind speed exponent of 0.4. Using this exponent, the model is tested against an independent data set. Subsequent agreement between wind speeds simultaneously determined by SAR and the Seasat-A Satellite Scatterometer (SASS) is within 0.7 m/s rms. A one-dimensional Fourier transform of the SAR-derived wind field shows an increasing energy content in rough agreement with the Van der Hoven spectrum.
Document ID
19810061706
Acquisition Source
Legacy CDMS
Document Type
Other - Collected Works
Authors
Jones, W. L. (NASA Langley Research Center Hampton, VA, United States)
Bracalente, E. M. (NASA Langley Research Center Hampton, VA, United States)
Delnore, V. E. (Kentron International, Inc. Hampton, VA, United States)