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A semiempirical model of the normalized radar cross section of the sea surface, 2. Radar modulation transfer function : Fluxes, surfaces waves, remote sensing, and ocean circulation in the North Mediterranean Sea: results from the FETCH experiment

TLDR
In this article, the authors developed a physical model that takes into account not only the Bragg mechanism but also the non-Bragg scattering associated with radio wave scattering from breaking waves.
Abstract
[1] Multiscale composite models based on the Bragg theory are widely used to study the normalized radar cross section (NRCS) over the sea surface. However, these models are not able to correctly reproduce the NRCS in all configurations. In particular, even if they may provide consistent results for vertical transmit and receive (VV) polarization, they fail in horizontal transmit and receive (HH) polarization. In addition, there are still important discrepancies between model and observations of the radar modulation transfer function (MTF), which relates the modulations of the NRCS to the long waves. In this context, we have developed a physical model that takes into account not only the Bragg mechanism but also the non-Bragg scattering associated with radio wave scattering from breaking waves. The same model was built to explain both the background NRCS and its modulation by long surface wave (wave radar MTF problem). In part 1, the background NRCS model was presented and assessed through comparisons with observations. In this part 2, we extend the model to include a third underlying scale associated with longer waves (wavelength ∼10-300 m) to explain the modulation of the NRCS. Two contributions are distinguished in the model, corresponding to the so-called tilt and hydrodynamic MTF. Results are compared to observations (already published in the literature or derived from the FETCH experiment). As found, taking into account modulation of wave breaking (responsible for the non-Bragg mechanism) helps to bring the model predictions in closer agreement with observations. In particular, the large MTF amplitudes for HH polarization (much larger than for VV polarization) and MTF phases are better interpreted using the present model.

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Dissertation

Étude de la rétrodiffusion des surfaces d'eau en bande Ka à faible incidence

TL;DR: In this article, a modelle de retrodiffusion (GO4) adapte a la configuration SWOT is presented, which conserves the precision du modele de reference de l’Optique Physique tout en gardant la simplicite du modelle plus couramment employe de l'Optique Geometrique.
References
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Journal ArticleDOI

Direct measurements of ocean surface velocity from space: Interpretation and validation

TL;DR: In this paper, the median Doppler shift of radar echoes is analyzed in measurements by ENVISAT's Advanced Synthetic Aperture Radar (ASAR) over the ocean, and a simple quantitative forward model is proposed, based on a practical two-scale decomposition of the surface geometry and kinematics.
Journal ArticleDOI

Microwave scattering and the straining of wind-generated waves

W. C. Keller, +1 more
- 01 Feb 1975 - 
TL;DR: In this article, the amplitude of a 0.575-Hz plunger-generated wave was measured in a wave tank as a function of air friction velocity and plunger wave amplitude.
Journal ArticleDOI

Turbulent shear flow over slowly moving waves

TL;DR: In this article, the authors investigate the changes to a fully developed turbulent boundary layer caused by the presence of a two-dimensional moving wave of wavelength L = 2π/k and amplitude a.
Journal ArticleDOI

The two-frequency microwave technique for measuring ocean-wave spectra from an airplane or satellite

TL;DR: In this paper, the authors investigated the applicability of the two-frequency microwave technique at slant incidence for the measurement of ocean wave spectra, first proposed by Rucket et al. (1972), with respect to its applicability in aircraft and space vehicles.
Journal ArticleDOI

On radar imaging of current features: 1. Model and comparison with observations

TL;DR: In this article, a new radar imaging model of ocean current features is proposed, which takes into account scattering from "regular" surfaces (by means of resonant Bragg scattering and specular reflections) and scattering from breaking waves.
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