Journal
GEOPHYSICAL RESEARCH LETTERS
Volume 42, Issue 22, Pages 9898-9905Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1002/2015GL065173
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Funding
- ONR [N0014-09-1-0392, DURIP N00014-09-0818]
- NSF [OCE-0526442]
- Clarence O. Collins' ASEE post-doctoral fellowship at the Naval Research Laboratory, Stennis Space Center
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Direct flux measurements of stress direction taken at the ocean surface during Typhoon Chaba (2010) over 3 days are examined for wind speeds between 12 and 26.5 m s(-1). Results show stress deviated up to 35 degrees from the wind direction and resided predominantly between the wind and peak wave directions in both bimodal and unimodal seas. Off-wind stress angle was most pronounced in Chaba's wake where wind sea and swell created an apparent unimodal system with narrow directional spread. These conditions lasted 2 days during which the stress direction was midway between the wind and wave directions. The implications for tropical cyclone forecasting are discussed.
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