Alexis Mouche

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—The synthetic aperture radar (SAR) Doppler cen-troid has been used to estimate the scatter line-of-sight radar velocity. In weak to moderate ocean surface current environment, the SAR Doppler centroid is dominated by the directionality and strength of wave-induced ocean surface displacements. In this paper, we show how this sea state signature can be used(More)
—The " galactic glitter " phenomenon at L-band, i.e., the scattering of celestial sky radiation by the rough ocean surface, is examined here as a potential source of error for sea surface salinity (SSS) remote sensing. We begin by considering the transformations that must be applied to downwelling celestial noise in order to compute the eventual impact on(More)
An analysis of radar observations in C band combined with models is proposed to study some of the ocean surface properties and their relation with the sea surface backscatter. The electromagnetic part of the models is of different kinds: composite Bragg model with or without including effect of wave breaking zones on the normalized radar cross-section(More)
Existing models for the shortwave spectrum of the sea surface are not consistent with microwave satellite data when multi-bands and multi-incidence data sets are considered. We devise a simple parametric model for the shortwave omnidirectional spectrum of the sea surface on the basis of a three-band (C, Ku, and Ka) and multi-incidence (low, moderate, and(More)
The possibility for retrieving wind fields from C-band synthetic aperture radar (SAR) data is well developed and validated and is currently used to produce operational wind maps. With the X-band SAR aboard the German TerraSAR-X and the L-band SAR aboard the Japanese ALOS, two additional frequencies have become available. It is quite possible that(More)