Titlebook: Radar Scattering from Modulated Wind Waves; Proceedings of the W G. J. Komen,W. A. Oost Conference proceedings 1989 Kluwer Academic Publish

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On the Changes in Phase Speed of One Train of Water Waves in the Presence of Anotherllips (1962). Agreement to 6 significant digits has been obtained between the calculations based on these two distinct methods. Full numerical results in the form of polar diagrams over a wide range of wavelengths, away from conditions of triad resonance, are provided.

AVOW

SAR Imaging of Ocean Waves in the Presence of Variable Currentsreader quickly up to date in the literature and still provide enough insight into the processes involved. Some new results on the development of the gravity-capillary wavenumber spectrum are also given.

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Calculation of Microwave Doppler Spectra from the Ocean Surface with a Time-Dependent Composite Modend H-H polarization, and its time dependence is based on the assumption of linear surface evolution. The width of the computed spectra increases with increasing radar frequency and decreasing incidence angle due primarily to the motion of the long-wave surface. This motion also produces a shift in t

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Limitations of the Two-Scale Theory for Microwave Backscatter from The Ocean flows over submerged sand banks). In addition appear a variety of man made objects (e.g. rigs, vessels) which may be sensed directly or via their effects on the oceanic environment (i.e. their wakes). An important part in the proper interpretation of such images is a thorough understanding of the s

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Effects of Reduced Surface Tension on Short Waves at Low Wind Speeds in a Fresh Water Laked from a model compound which reduced surface tension by 6–8 mN/m, formed 10 m patches which drifted by the wave sensor in 3–5 minutes. Naturally forming slicks, reducing surface tension by 1 to 2.8 mN/m, were also observed. For wind speeds of 2–3 m/s, waves of intrinsic frequency greater than about

Musculoskeletal

Temporal and Spatial Variability of the Wind Stress Vectorsurface. These periodicities, illustrated by measurements collected during a number of recent field experiments, indicate that the inertial time scale, planetary boundary layer (PBL) rolls, and dominant wavelengths of surface gravity waves and swell become important in interpreting stress estimates.

玩笑

Energy Balance in Small-Scale Waves — An Experimental Approach Using Optical Slope Measuring Techniqre obtained with a laser slope gauge and image sequences of the wave slope with an imaging slope gauge. Frequency spectra, wavenumber spectra, and wavenumber-frequency spectra are calculated from data obtained in different wind/wave facilities. They show a strong nonlinearity of the waves already fo