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Ocean Surface's Scattering Coefficient Retrieval by Delay–Doppler Map Inversion

机译:时延-多普勒地图反演反演海面散射系数

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摘要

Global navigation satellite system reflectometry of signals is a promising technique to remotely sense a number of Earth's geophysical parameters, and it has been proposed for ocean monitoring applications such as mesoscale altimetry or sea state monitoring. So far, the following two main approaches have been considered to retrieve a sea state descriptor from measured delay waveforms or delay–Doppler (DD) maps (DDMs): 1) fitting the measurements to a model tuned with the desired parameter or 2) directly linking a property of the measurements with the parameter to be retrieved (e.g., volume of the normalized DDM). However, these approaches provide a single sea state descriptor related to the overall glistening zone where sea state conditions may not be homogeneous. In this letter, the relationship between the physical space and the DD domains is exploited, and a method to retrieve the bistatic scattering coefficient distribution over the observation ocean surface from measured DDMs is proposed.
机译:全球导航卫星系统的信号反射法是一种有前景的技术,可用于遥感许多地球的地球物理参数,并且已被提议用于海洋监测应用,如中尺度测高或海况监测。到目前为止,已经考虑了以下两种主要方法来从测得的延迟波形或延迟多普勒(DD)映射(DDM)中检索海况描述符:1)将测量值拟合到使用所需参数调整的模型,或者2)直接将测量的属性与要检索的参数(例如,归一化DDM的体积)关联起来。然而,这些方法提供了与整个闪耀区有关的单个海况描述符,其中海况条件可能不均匀。在这封信中,利用了物理空间和DD域之间的关系,并提出了一种从测得的DDM中检索观测海洋表面双基地散射系数分布的方法。

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