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On the Discrimination of Radar Signatures of Atmospheric Gravity Waves and Oceanic Internal Waves on Synthetic Aperture Radar Images of the Sea Surface

机译:关于海面合成孔径雷达图像上大气重力波和海洋内波的雷达特征的区分

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摘要

Synthetic aperture radar (SAR) images acquired over the ocean frequently show sea wave-like patterns that have wavelengths well above those of ocean surface waves and that are sea surface signatures of oceanic internal waves (OIWs) or of atmospheric gravity waves (AGWs). However, it is often difficult to decide whether they result from the first or the second kind of waves, which has led many investigators to misinterpret SAR images of the sea surface. Based on solitary wave and radar imaging theories of AGWs and OIWs, we present criteria that help distinguish between them. However, there are cases where these criteria, which are based solely on the shape and structure of the features visible on the SAR images, yield ambiguous results. In these cases, one must resort to additional information on the generation of AGWs and OIWs, which are listed in this paper.
机译:在海洋上获取的合成孔径雷达(SAR)图像经常显示出类似于海浪的图案,其波长远高于海面波的波长,并且是海洋内部波(OIW)或大气重力波(AGW)的海面信号。但是,通常很难确定它们是由第一波还是第二波引起的,这导致许多研究人员误解了海面的SAR图像。基于AGW和OIW的孤立波和雷达成像理论,我们提出了有助于区分它们的标准。但是,在某些情况下,仅基于SAR图像上可见特征的形状和结构的这些标准会产生模棱两可的结果。在这种情况下,必须诉诸于本文列出的有关AGW和OIW生成的其他信息。

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