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• W3106098497 abstract "Empirical relations for the wind-induced drift current, Ud, measured at a wavy water surface in a laboratory and in the field, are presented and discussed. A relatively large value of Ud with respect to the friction velocity in water is highlighted, and it is noted that the empirical relations are incomplete, as they do not describe the drift-current dependence on surface-wave parameters. With the purpose of theoretical justification of these empirical facts, a semi-phenomenological model for the wind-induced drift current is constructed. It is based on the known theoretical results and empirical data related to the three-layer structure of the wavy air–water interface, which includes: (i) the air boundary layer, (ii) the wave zone, and (iii) the water boundary layer. The linear profile of drift current Ud(z), found empirically in the wave zone, allows the general relation for Ud to be determined. It is based on the equation of balance between the wind-induced momentum flux, τ, and the vertical gradient of drift current dUd(z)/dz in the wave zone. The model provides interpretation of the empirical results and indicates a means for their further specification." @default.
• W3106098497 created "2020-11-23" @default.
• W3106098497 creator A5027327960 @default.
• W3106098497 date "2019-05-29" @default.
• W3106098497 modified "2023-10-16" @default.
• W3106098497 title "A Semi-phenomenological Model for Wind-Induced Drift Currents" @default.
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• W3106098497 doi "https://doi.org/10.1007/s10546-019-00456-1" @default.
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