1992
DOI: 10.1029/91jc01876
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Surface films and wind wave growth

Abstract: The generation and growth of surface water waves by the wind and including modified boundary conditions appropriate for the presence of surfactants at the surface are reconsidered using linear instability theory to describe the process. The new features of our work are the inclusion of both surfactants and a wind drift layer. We allow a coupled mean flow in both the air and water; the depth‐dependent mean flow is considered to be wind‐induced. The complex wave frequencies are determined numerically. Uncontroll… Show more

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Cited by 12 publications
(6 citation statements)
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“…A rigorous theoretical analysis of wind wave growth in the presence of a surface film is given by [39]. Further consideration of ( 5) and ( 6) sheds light on the general damping mechanism.…”
Section: A Radar Backscatter From the Ocean Surfacementioning
confidence: 99%
“…A rigorous theoretical analysis of wind wave growth in the presence of a surface film is given by [39]. Further consideration of ( 5) and ( 6) sheds light on the general damping mechanism.…”
Section: A Radar Backscatter From the Ocean Surfacementioning
confidence: 99%
“…Field and laboratory experiments (Cox & Munk 1954;Lombardini et al 1989;Barger et al 1970;Hühnerfuss et al 1983;Ermakov et al 1986;Tang & Wu 1992;Bock et al 1999;Uz et al 2002;Mitsuyasu & Honda 1984) have shown that surfactants reduce the high-frequency part of the windwave spectrum. The effects of the film elasticity and surface viscosity on wind-wave growth and damping rates were studied numerically by Creamer & Wright (1992), who showed that the damping rate is substantially increased by the film elasticity and that the effect of the surface viscosity is more pronounced at larger wavenumbers when the surface elasticity is small. Lucassen (1981) demonstrated that the surfacedilational modulus has a considerable effect on the damping of short gravity waves and gravity capillary waves.…”
Section: Introductionmentioning
confidence: 99%
“…The change in surface tension can also affect the longer wavelength components of the ocean wave spectrum through gradients in the surface tension (Marangoni effect) and indirectly through nonlinear wave-wave interactions that shift energy between different wavenumber components of the spectrum [Alpers and Hühnerfuss, 1988;Gade et al, 1998aGade et al, , 1998b. A rigorous theoretical analysis of wind wave growth in the presence of a surface film is given by Creamer and Wright [1992].…”
Section: Theory Of Radar Response To Oil On Watermentioning
confidence: 99%