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New insights into the radar backscattering from the water surface at different radar frequencies and polarizations in the presence of rain and wind

机译:在有雨和风的情况下,在不同的雷达频率和极化下,雷达从水面向后散射的新见解

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In order to interpret different radar contrasts on images of rain events over the ocean acquired by a multi-frequency/multi-polarization synthetic aperture radar (SAR), laboratory and field measurements have been performed. The aim of this investigation is to develop a method for estimating rain rates of small scale rain events over the ocean using radar backscatter data. The radar backscatter measurements of the water surface during the field experiments have been carried out using a four-frequency/multi-polarization scatterometer, during the laboratory measurements using a 9.8 GHz (X band) scatterometer at the wind wave tank of the University of Hamburg under different wind and rain conditions. The authors compare the results of these measurements with the radar cross-sections derived from SAR-images of rain cells over the ocean by calculating the ratios of the radar cross-sections at co- and cross-polarization (CCP-ratios). With help of further calculations performed using a composite surface model, and some basic assumptions the authors interpret radar images of rain cells more quantitatively by giving first estimates of rain rates.
机译:为了解释由多频/多极化合成孔径雷达(SAR)采集的海洋降雨事件图像的不同雷达对比,已经进行了实验室和现场测量。这项研究的目的是开发一种使用雷达反向散射数据估算海洋小规模降雨事件的降雨率的方法。在汉堡大学的风波箱中,使用9.8 GHz(X波段)散射仪在实验室测量期间,使用四频/多极化散射仪在野外实验期间对水表面进行了雷达背向散射测量。在不同的风雨条件下。作者通过计算共极化和交叉极化时雷达横截面的比率(CCP比率),将这些测量结果与从海洋上的雨单元的SAR图像得出的雷达横截面进行了比较。借助于使用复合表面模型进行的进一步计算以及一些基本假设,作者通过给出初次的降雨率估算,更加定量地解释了降雨单元的雷达图像。

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