Abstract
Open ocean measurements at both shallow and deep depths show that ambient acoustic noise above 10–15 kHz increases nearly linearly as the log of the wind speed. This relationship is studied under a variety of wind/sea conditions at 15, 20, and 25 kHz bands using a newly developed self‐contained ambient noise recorder (SCANR). Assessment is made of possible ambient noise prediction from wind speed data obtained from a satellite mounted microwave scatterometer.
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