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The Transition from...
The Transition from Downward to Upward Air–Sea Momentum Flux in Swell-Dominated Light Wind Conditions
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- Högström, Ulf (författare)
- Uppsala universitet,Luft-, vatten- och landskapslära
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- Sahlée, Erik (författare)
- Uppsala universitet,Luft-, vatten- och landskapslära
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- Smedman, Ann-Sofi, 1942- (författare)
- Uppsala universitet,Luft-, vatten- och landskapslära
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- Rutgersson, Anna, 1971- (författare)
- Uppsala universitet,Luft-, vatten- och landskapslära
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- Nilsson, Erik O., 1983- (författare)
- Uppsala universitet,Luft-, vatten- och landskapslära
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- Kahma, Kimmo (författare)
- FMI
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- Drennan, William (författare)
- University of Miami, RSMAS
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(creator_code:org_t)
- 2018
- 2018
- Engelska.
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Ingår i: Journal of the Atmospheric Sciences. - 0022-4928 .- 1520-0469. ; 75:8, s. 2579-2588
- Relaterad länk:
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https://urn.kb.se/re...
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https://doi.org/10.1...
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Abstract
Ämnesord
Stäng
- Fifteen hours of consecutive swell data from the experiment Flux, État de la Mer, et Télédétection en Condition de Fetch Variable (FETCH) in the Mediterranean show a distinct upward momentum flux. The characteristics are shown to vary systematically with wind speed. A hysteresis effect is found for wave energy of the wind-sea waves when represented as a function of wind speed, displaying higher energy during decaying winds compared to increasing winds. For the FETCH measurements, the upward momentum transfer regime is found to begin for wind speeds lower than about U 5 4ms21 . For the lowest observed wind speeds U , 2.4 m s21 , the water surface appears to be close to dynamically smooth. In this range almost all the upward momentum flux is accomplished by the peak in the cospectrum between the vertical and horizontal components of the wind velocity. It is demonstrated that this contribution in turn is linearly related to the swell significant wave height Hsd in the range 0.6 , Hsd , 1.4 m. For Hsd , 0.6 m, the contribution is zero in the present dataset but may depend on the swell magnitude in other situations. It is speculated that the observed upward momentum flux in the smooth regime, which is so strongly related to the cospectral peak at the dominant swell frequency, might be caused by the recirculation mechanism found by Wen and Mobbs in their numerical simulation of laminar flow of a nonlinear progressive wave at low wind speed
Ämnesord
- NATURVETENSKAP -- Geovetenskap och miljövetenskap -- Meteorologi och atmosfärforskning (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences -- Meteorology and Atmospheric Sciences (hsv//eng)
Nyckelord
- Air-sea interaction; Atmosphere-ocean interaction; Momentum
- Meteorologi
- Meteorology
Publikations- och innehållstyp
- ref (ämneskategori)
- art (ämneskategori)
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