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Surface roughness and breaking wave properties retrieved from polarimetric microwave radar

机译:从极化微波雷达获取的表面粗糙度和断波特性

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摘要

Ocean surface roughness and wave breaking are the two main contributors of radar backscattering from the ocean surface. The relative weightings of the two contributions vary with the microwave polarization: the VV (vertical transmit vertical receive) is dominated by the Bragg resonance scattering mechanism, and the HH (horizontal transmit horizontal receive) and VH (horizontal transmit vertical receive or vertical transmit horizontal receive) contain nontrivial non-Bragg contributions mainly produced by breaking features. A method is developed to obtain the short-scale properties of ocean surface roughness and wave breaking from Ku, C, and L band polarimetric sea returns. The results are used for quantitative evaluation of the ocean surface roughness spectral models and for deriving understanding of the breaking contribution important to microwave ocean remote sensing, in particular its dependence on wind speed, microwave frequency, and incidence angle. Implications of the results to air-sea interaction applications are discussed.
机译:海洋表面粗糙度和波浪破碎是雷达从海洋表面反向散射的两个主要因素。这两个分量的相对权重随微波极化而变化:VV(垂直发射垂直接收)受布拉格共振散射机制支配,HH(水平发射水平接收)和VH(水平发射垂直接收或水平发射水平)接收)包含主要是由破坏特征产生的非平凡的非布拉格贡献。开发了一种方法,用于从Ku,C和L波段极化海返回获得海洋表面粗糙度和波浪破碎的短尺度特性。结果用于海洋表面粗糙度光谱模型的定量评估,并用于理解对微波海洋遥感重要的突破性贡献的理解,尤其是其对风速,微波频率和入射角的依赖性。讨论了结果对海-气相互作用应用的影响。

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