Titlebook: Simulation of the Sea Surface for Remote Sensing; Alexander Zapevalov,Konstantin Pokazeev,Tatiana Ch Book 2021 The Editor(s) (if applicabl

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Statistical Distributions Sea Surface Slope,es not disturb the sea surface and has a high spatial resolution is a laser slopemeter. Chapter . analyses the variability of sea surface slope measured by a laser slopemeter on a stationary oceanographic platform.

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On the Dispersion Relation of Sea Waves,s chapter, on the basis of measurements made on the oceanographic platform, the stability of phase relations in sea waves is analyzed. The models describing the phase relations and the quadratic coherence function in a multicomponent wave field are constructed.

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Effect of Long Surface Waves on the Bragg Scattering of Microwave,Quantitative estimates of backscatter cross-section variation for probing on horizontal and vertical polarization are obtained. Differences in statistical distributions of sea surface slopes from Gaussian distributions are taken into account in the analysis.

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Study of the Variability in the Ocean-Atmosphere Interface as a Reflective Surface of Light, were stochastically related to the parameters of short gravitational and gravity-capillary waves. The dependencies connecting the optical characteristics of the sea surface with its dynamic parameters and with the wind speed were constructed.

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Statistical Distributions Sea Surface Slope,hat characterize the roughness are the slope of the sea surface. The problem of studying the slope variability is that the main contribution to their variance are short waves, whose characteristics are technically difficult to measure under field conditions. The most effective measuring tool that do

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On the Dispersion Relation of Sea Waves, and temporal structure of the surface wave field has become very important. When interpreting remote sensing data it is necessary to take into account the nonlinearity of sea waves, especially the function of angular distribution, describing the distribution of wave energy in the directions. In thi

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Modeling the Shape of the Impulse Reflected from the Sea Surface, observed in field conditions and the excited sea surface elevation distribution kurtosis on the accuracy of sea surface level recovery along the satellite route is estimated. The possibilities and limitations of using a truncated Gram–Charlier distribution for building the probability density funct

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Effect of Long Surface Waves on the Bragg Scattering of Microwave,s always propagate along curvilinear surfaces created by longer waves. Analysis of the effects produced by long waves is based on direct in situ measurements of sea surface slopes made with a laser slopemeter. Situations where probing is performed in centimetre and millimetre ranges are considered.