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- W2181760414 abstract "In the present work, we investigate the geometric properties of wind waves at the different stages of wave development as observed in the large IRPHE-Luminy wind wave tank for a wide range of wind speeds and fetches. Visualizations of gravity-capillary to gravity-scale wave profiles in the alongwise direction were performed simultaneously with single-point wave elevation and slope measurements. The air flow velocity field and the surface wind stress were monitored by a Pitot tube and X-wire probes located at the immediate vicinity of the wave probes. At first, these observations show at a given wind speed, the dominant wave mean square slope (mss) is strongly wave scale dependent, its amplitude and its angular width both reaching a maximum at an intermediate wave scale. The large decrease in dominant wave mss following the overshoot may be explained by a sharp increase in wave dissipation due to microbreaking and breaking, both responsible of an intense generation of widely spread capillaries. As a result, the dominant wave mean square slope increases regularly with wind forcing when the wave field is well-developed but decreases slowly for highly-forced wave fields. Consistently, the dominant wave skewness and kurtosis are found to vary with wind forcing but in less extent. The direct impact of wind forcing on short gravity-scale breaking wave features is then investigated in a more deterministic way from the analysis of wave profile images. The relevance of these observations for high wind conditions at sea is then discussed. * in stay at the Laboratoire d'Oceanographie Spatiale, Ifremer-Brest, Plouzane, France until June 30, 2010." @default.
- W2181760414 created "2016-06-24" @default.
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- W2181760414 date "2010-01-01" @default.
- W2181760414 modified "2023-09-27" @default.
- W2181760414 title "Impact of wind forcing on wind wave shape and breaking" @default.
- W2181760414 hasPublicationYear "2010" @default.
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