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Open AccessJournal ArticleDOI

Quad‐polarization SAR features of ocean currents

TLDR
In this paper, a methodology is demonstrated to exploit the polarization sensitivity of high-resolution radar measurements to interpret and quantify upper ocean dynamics, where the polarized Bragg-type radar scattering is isolated by considering the difference (PD) between vertically and horizontally polarized radar signals.
Abstract
A methodology is demonstrated to exploit the polarization sensitivity of high-resolution radar measurements to interpret and quantify upper ocean dynamics. This study particularly illustrates the potential of quad-polarization synthetic aperture radar (SAR) measurements. The analysis relies on essential characteristics of the electromagnetic scattering mechanisms and hydrodynamical principles. As the relaxation scale of centimeter-scale ocean surface scatters is typically small, radar signal anomalies associated with surface manifestations of the upper ocean dynamics on spatial scales exceeding 100 m are mostly dominated by nonresonant and nonpolarized scatters. These “scalar” contributions can thus efficiently trace local breaking and near-breaking areas, caused by surface current variations. Using dual copolarized measurements, the polarized Bragg-type radar scattering is isolated by considering the difference (PD) between vertically and horizontally polarized radar signals. The nonpolarized (NP) contribution associated with wave breaking is then deduced, using the measured polarization ratio (PR) between polarized signals. Considering SAR scenes depicting various surface manifestations of the upper ocean dynamics (internal waves, mesoscale surface current features, and SST front), the proposed methodology and set of decompositions (PD, PR, and NP) efficiently enable the discrimination between surface manifestation of upper ocean dynamics and wind field variability. Applied to quad-polarized SAR images, such decompositions further provide unique opportunities to more directly assess the cross-polarized (CP for HV or VH) signal sensitivity to surface roughness changes. As demonstrated, such an analysis unambiguously demonstrates and quantitatively evaluates the relative impact of breakers on cross-polarized signals under low to moderate wind conditions.

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Citations
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Journal ArticleDOI

Combined Co- and Cross-Polarized SAR Measurements Under Extreme Wind Conditions

TL;DR: This paper opens perspectives for MetOp-SG SCA, the next-generation C-band scatterometer with co- and cross-polarization capability, and shows that the decrease in resolution does not dramatically change the sensitivity difference between VV and VH polarizations.
Journal ArticleDOI

Global C-Band Envisat, RADARSAT-2 and Sentinel-1 SAR measurements in copolarization and cross-polarization

TL;DR: In this paper, a global analysis of ENVISAT and Sentinel-1 synthetic aperture radar (SAR) measurements helps to refine, at medium resolution (tens of kilometers) and especially for HH configuration, a C-band geophysical model function (GMF) to analyze wind sensitivity for different incidence and azimuth angles.
BookDOI

Oceanic Internal Tides: Observations, Analysis and Modeling

TL;DR: In this paper, the structure and variability of internal tides and their geographical distribution in the ocean are studied. But the most important idea presented in this paper is the strong generation of internal tide over submarine ridges.
References
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Journal ArticleDOI

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

TL;DR: 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.
Journal ArticleDOI

Spectral and statistical properties of the equilibrium range in wind-generated gravity waves

TL;DR: In this paper, the nature of the equilibrium range is reexamined, using the dynamical insights into wave-wave interactions, energy input from the wind and wave-breaking that have been developed since 1960.
Journal ArticleDOI

The Dynamics of the Upper Ocean

J Crease
- 01 May 1967 - 
TL;DR: In the last decade the theory of ocean surface waves has expanded greatly from the firm foundations of Lamb's Hydrodynamics as mentioned in this paper, and the oceanographer's and meteorologist's need to understand the energy transfer through the sea surface and between one part of the ocean and another has provided stimulus for these and other theoretical studies
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