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- W3082789898 abstract "Abstract Buoy observations from a 1999 Gulf of Mexico field program (GOM99) are used to investigate the relationships among friction velocity u * , wind speed U , and amount of swell present. A U – u *sea parameterization is developed for the case of pure wind sea (denoted by u *sea ), which is linear in U over the range of available winds (2–16 m s −1 ). The curve shows no sign of an inflection point near 7–8 m s −1 as suggested in a 2012 paper by Andreas et al. on the basis of a transition from smooth to rough flow. When observations containing more than minimal swell energy are included, a different U – u * equation for U < 8 m s −1 is found, which would intersect the pure wind-sea curve about 7–8 m s −1 . These two relationships yield a bilinear curve similar to Andreas et al. with an apparent inflection near 7–8 m s −1 . The absence of the inflection in the GOM99 experiment pure wind-sea curve and the similarity of the GOM99 swell-dominated low wind speed to Andreas et al.’s low wind speed relationship suggest that the inflection may be due to the effect of swell and not a flow transition. Swell heights in the range of only 25–50 cm may be sufficient to impact stress at low wind speeds." @default.
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- W3082789898 date "2020-11-01" @default.
- W3082789898 modified "2023-09-27" @default.
- W3082789898 title "Effect of Swell on Wind Stress for Light to Moderate Winds" @default.
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- W3082789898 doi "https://doi.org/10.1175/jas-d-19-0338.1" @default.
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