Titlebook: Surface Waves and Fluxes; Volume II — Remote S G. L. Geernaert,W. L. Plant Book 1990 Kluwer Academic Publishers 1990 Ocean.Wind speed.remot

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Electromagnetic Scattering from the Sea at Low Grazing Angles,der these conditions it is expected that the surface might often be deeply shadowed, yet the experimental evidence is unclear, sometimes even contradictory. It is obvious that this is a very special scattering regime, in which the conventional ideas of sea scatter are quite possibly of little use. A

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Microwave Techniques for Measuring Directional Wave Spectra,to measure, either directly or indirectly, the surface elevation at a given location in space as a function of time. The observed temporal fluctuations of the surface elevation are described statistically in terms of the frequency spectrum. Using the dispersion relation for surface gravity waves, ea

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Passive Microwave Remote Sensing of Ocean Surface Wind Speed,ic emission from the ocean depends upon the degree of surface roughness. Because the ocean surface becomes rougher with increasing wind speed, a potential technique became available for the global monitoring of surface winds from earth orbiting satellites. The qualitative nature of the theoretical r

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Book 1990ted compendium of air-sea interaction theory to be organized, developed, and published. Many new results were emerging at the time, i.e., results from the MARSEN, MAS EX, MILDEX, and TOWARD field projects (among others) were in the process of being reported and/or published. Further, a series of new

Exposition

Dependence of Radar Backscatter on Environmental Parameters, waves and the characteristics of radar backscatter so as to be able to obtain the winds. Any environmental feature of the waves that causes backscatter to change other than those due to some well defined property of the local wind can cause the backscatter to vary in a way not directly related to the local wind.