Coupled dynamics of short waves and the airflow over long surface waves

[1] A study is presented of modulations induced by a dominant long surface wave (LW) in the coupled airflow–short wind-generated waves (SW) system. The modulation of SWs in the gravity range results from their interaction with the LW orbital velocity and their interaction with the wind stress modulated by the LW. The modulation of waves in the capillary range is mainly due to the modulation of the rate of generation of parasitic capillaries by steep short gravity waves. The variation of the wind surface stress is described by the dynamics of the turbulent airflow over the LW with the surface roughness varying along its profile. The variation of the surface roughness is caused by the variation of the form drag supported by modulated SWs. In turn, the LW-induced variation of the surface stress affects the SW modulation. This provides a feedback in the coupled airflow–SW system in the presence of the LW. The model results show that the amplitude of the surface roughness modulation can be large. In terms of the modulation transfer function (MTF), it can reach values of 10–20. The modulation of the form drag, which causes the modulation of the surface roughness, comes mainly from short breaking waves strongly modulated by dominant waves. The modulation of the surface roughness considerably affects the dynamics of the airflow over the LW and thus the LW wind growth rate. Models of the airflow above waves assuming a constant roughness parameter underestimate the growth rate parameter approximately two to three times as compared to the measured values. The present study shows that when the variation in the surface roughness is accounted for, the growth rate parameter increases roughly twice, which to a large extent reduces the discrepancy with measurements.

[1]  C. Mastenbroek,et al.  Drag of the sea surface , 1995 .

[2]  A. Townsend Flow in a deep turbulent boundary layer over a surface distorted by water waves , 1972, Journal of Fluid Mechanics.

[3]  P. Gent,et al.  A numerical model of the air flow above water waves , 1976, Journal of Fluid Mechanics.

[4]  R. W. Stewart The air-sea momentum exchange , 1974 .

[5]  O. Shemdin,et al.  Measurement of the hydrodynamic modulation of centimeter waves , 1991 .

[6]  C. Cox Statistics of the sea surface derived from sun glitter , 1954 .

[7]  O. Phillips Spectral and statistical properties of the equilibrium range in wind-generated gravity waves , 1985, Journal of Fluid Mechanics.

[8]  V. Kudryavtsev,et al.  The Impact Of Air-Flow Separation On The Drag Of The Sea Surface , 2001 .

[9]  P. K. Taylor,et al.  Wind stress measurements from the open ocean , 1996 .

[10]  C. Mastenbroek,et al.  Experimental evidence of the rapid distortion of turbulence in the air flow over water waves , 1996, Journal of Fluid Mechanics.

[11]  S. Belcher,et al.  Turbulent shear flow over slowly moving waves , 1993, Journal of Fluid Mechanics.

[12]  K. Hasselmann,et al.  The two-frequency microwave technique for measuring ocean-wave spectra from an airplane or satellite , 1978 .

[13]  B. Chapron,et al.  A semiempirical model of the normalized radar cross‐section of the sea surface 1. Background model , 2003 .

[14]  Bertrand Chapron,et al.  Coupled sea surface-atmosphere model: 2. Spectrum of short wind waves , 1999 .

[15]  W. Plant A relationship between wind stress and wave slope , 1982 .

[16]  R. Long,et al.  Array measurements of atmospheric pressure fluctuations above surface gravity waves , 1981, Journal of Fluid Mechanics.

[17]  C. Mastenbroek,et al.  MODULATION OF WIND RIPPLES BY LONG SURFACE WAVES VIA THE AIR FLOW: A FEEDBACK MECHANISM , 1997 .

[18]  William J. Plant,et al.  Hydrodynamic modulation of short wind‐wave spectra by long waves and its measurement using microwave backscatter , 1994 .

[19]  O. Phillips The dynamics of the upper ocean , 1966 .

[20]  V. Kudryavtsev The coupling of wind and internal waves: modulation and friction mechanisms , 1994, Journal of Fluid Mechanics.

[21]  J. F. Meirink,et al.  Simplified Model Of The Air Flow Above Waves , 2001 .

[22]  W. Alpers,et al.  A three‐scale composite surface model for the ocean wave–radar modulation transfer function , 1994 .