Two-dimensional wave number spectra of small-scale water surface waves

Two-dimensional wave slope spectra have been measured in the large Delft wind-wave facility using an imaging optical technique and digital image processing. The data cover wavelengths from 0.4 to 24cm and wind speeds (U10) from 2.7 to 17.2 ms−1. The spectral densities of small gravity waves at higher wind speeds are proportional to k−3.5 and u*. Capillary-gravity and capillary waves show features which clearly manifest that the energy balance for these waves is much different from that for gravity waves. The degree of saturation is approximately constant at a given wind speed, but strongly increases with friction velocity (∝ u*2.5). A sharp cutoff, which is almost independent of the wind speed, occurs at a wavelength of about 7 mm.

[1]  Roman E. Glazman,et al.  Effects of sea maturity on satellite altimeter measurements , 1990 .

[2]  Stefan Waas,et al.  Optical Measuring Technique For Small Scale Water Surface Waves , 1989, Other Conferences.

[3]  W. Alpers,et al.  The damping of ocean waves by surface films: A new look at an old problem , 1989 .

[4]  John Trinder,et al.  Wavenumber spectra of short gravity waves , 1989, Journal of Fluid Mechanics.

[5]  W. A. Oost,et al.  Radar Scattering from Modulated Wind Waves , 1989 .

[6]  W. Plant General Discussion on the Energy Balance in Short Wind Waves , 1989 .

[7]  W. Rosenthal Derivation of Phillips α-Parameter from Turbulent Diffusion as a Damping Mechanism , 1989 .

[8]  Bernd Jähne Energy Balance in Small-Scale Waves — An Experimental Approach Using Optical Slope Measuring Technique and Image Processing , 1989 .

[9]  Paul Snoeij,et al.  First Results of the Viers-1 Experiment , 1989 .

[10]  Omar H. Shemdin,et al.  Directional measurement of short ocean waves with stereophotography , 1988 .

[11]  G. G. Pihos,et al.  Scatterometer wind speed bias induced by the large-scale component of the wave field , 1988 .

[12]  M. Donelan,et al.  Radar scattering and equilibrium ranges in wind‐generated waves with application to scatterometry , 1987 .

[13]  B. Jähne,et al.  On the parameters influencing air‐water gas exchange , 1987 .

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

[15]  William J. Plant,et al.  The dependence of X band microwave sea return on atmospheric stability and sea state , 1985 .

[16]  W. Oost The Pressure Anemometer—an Instrument for Adverse Circumstances , 1983 .

[17]  G. P. Loor Tower‐mounted radar backscatter measurements in the North Sea , 1983 .

[18]  B. Gotwols,et al.  Two-dimensional optical measurement of wave slope. , 1983, Applied optics.

[19]  S. Kitaigorodskii,et al.  On the Theory of the Equilibrium Range in the Spectrum of Wind-Generated Gravity Waves , 1983 .

[20]  Bernd Jähne,et al.  Comparison between an amplitude-measuring wire and a slope-measuring laser water wave gauge , 1982 .

[21]  W. Pierson,et al.  The relationship between wind vector and normalized radar cross section used to derive SEASAT‐A satellite scatterometer winds , 1982 .

[22]  H. L. Grant,et al.  A fast response surface-wave slope meter and measured wind-wave moments , 1977 .

[23]  R. Anderson,et al.  Laser instrument for detecting water ripple slopes. , 1973, Applied optics.

[24]  D. Stilwell,et al.  Directional energy spectra of the sea from photographs , 1969 .

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

[26]  L. McGoldrick Resonant interactions among capillary-gravity waves , 1965, Journal of Fluid Mechanics.

[27]  O. Phillips The equilibrium range in the spectrum of wind-generated waves , 1958, Journal of Fluid Mechanics.