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Theories for the interaction of electromagnetic and oceanic waves — A review

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TLDR
In this article, a review of analytical methods in electromagnetic scattering theory (i.e., geometrical and physical optics, perturbation, iteration, and integral-equation) which are applicable to the problems of remote sensing of the ocean is presented.
Abstract
This paper reviews analytical methods in electromagnetic scattering theory (i.e., geometrical and physical optics, perturbation, iteration, and integral-equation) which are applicable to the problems of remote sensing of the ocean. In dealing with Earth's surface (in this case, the weakly non-linear ocean), it is not possible to have a complete and exact description of its spatial and temporal statistics. Only the first few moments are generally available; and in the linear approximation the statistics are assumed homogeneous, stationary and Gaussian. For this case, the high-frequency methods (geometrical and physical optics) and perturbation (Rayleigh-Rice), or a combination of them, provide tractable analytical results (i.e., the specular-point, the slightly-rough Bragg scattering and the composite-surface models). The applicability and limitations of these models are discussed. At grazing incidence and for higher frequencies, other scattering mechanisms become significant; and shadowing, diffraction and trapping must be considered. The more exact methods (integral-equation and Green's function) have not been as successful in yielding tractable analytical solutions, although they have the potential to provide improved theoretical scattering results in the future.

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Citations
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Journal ArticleDOI

Scattering of GPS signals from the ocean with wind remote sensing application

TL;DR: A theoretical model that describes the power of a scattered GPS signal as a function of geometrical and environmental parameters has been developed, suggesting mapping of the wave-slope probability distribution in a synthetic-aperture-radar (SAR) fashion to allow more accurate measurements of wind velocity and wind direction.
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Radar scattering and equilibrium ranges in wind‐generated waves with application to scatterometry

TL;DR: In this paper, a model for the response of surface waves in the gravity-capillary equilibrium region of the spectrum is proposed on the basis of a local (in wavenumber) balance between wind input and dissipation.
Journal ArticleDOI

On the detectability of ocean surface waves by real and synthetic aperture radar

TL;DR: In this article, it is shown that for a relative small range of ocean wave parameters, the likelihood that the transfer function is linear increases as the direction of wave propagation approaches the range direction, as the wavelength increases, and as the wave height decreases.
Journal ArticleDOI

Theory of synthetic aperture radar ocean imaging: A MARSEN view

TL;DR: In this article, the authors reviewed basic synthetic aperture radar (SAR) theory of ocean wave imaging mechanisms, using both known work and recent experimental and theoretical results from the Marine Remote Sensing (MARSEN) Experiment.
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A three-dimensional analysis of marine radar images for the determination of ocean wave directionality and surface currents

TL;DR: In this paper, a series of spatial wave images recorded by a conventional marine radar is analyzed to determine the three-dimensional E(kx, ky, ω) spectrum.
References
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Book

The scattering of electromagnetic waves from rough surfaces

TL;DR: The scattering of electromagnetic waves from rough surfaces PDF is available at the online library of the University of Southern California as mentioned in this paper, where a complete collection of electromagnetic wave from rough surface books can be found.

Measurements of wind-wave growth and swell decay during the Joint North Sea Wave Project (JONSWAP)

TL;DR: In this article, wave spectra were measured along a profile extending 160 kilometers into the North Sea westward from Sylt for a period of two weeks in 1968 and 1969, with particular emphasis on wave growth under stationary offshore wind conditions and the attenuation of swell in water of finite depth.
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Measurement of the Roughness of the Sea Surface from Photographs of the Sun’s Glitter

TL;DR: In this paper, a method was developed for interpreting the statistics of the sun's glitter on the sea surface in terms of the statistic of the slope distribution, which was applied to aerial photographs taken under carefully chosen conditions in the Hawaiian area.
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