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- W2000381063 abstract "Measurements of velocity and scalar fluctuations were made using a stable platform in Bass Strait at a height of ∼5 m above the mean surface of the ocean. These measurements were obtained over a period of time where the wind velocity increased steadily before reaching an approximately constant value that was maintained for a duration of ∼10 h. During the initial period of the experiment, induced wave fluctuations, centered about the dominant wave frequency, are observed an spectra of the longitudinal u and vertical w velocity fluctuations, and on the uw cross spectrum. The cross spectrum indicates a relatively important transfer of momentum in the direction sea to air, at the wave frequency. No measurable wave influence is detected on either temperature θ or humidity q spectra, but wθ and wq cross spectra are either negligible or show a change of sign at the wave frequency. Although the effect on w persists, wave-induced disturbances on the cross spectra are small enough to be neglected when the ratio of wave phase speed to friction velocity becomes smaller than ∼40." @default.
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- W2000381063 date "1980-04-01" @default.
- W2000381063 modified "2023-09-26" @default.
- W2000381063 title "Wind-Wave-Induced Disturbances in the Marine Surface Layer" @default.
- W2000381063 doi "https://doi.org/10.1175/1520-0485(1980)010<0611:wwidit>2.0.co;2" @default.
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