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Polarimetric microwave wind radiometer model function and retrieval testing for WindSat

机译:极化微波风辐射计模型功能和WindSat的检索测试

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A geophysical model function (GMF), relating the directional response of polarimetric brightness temperatures to ocean surface winds, is developed for the WindSat multifrequency polarimetric microwave radiometer. This GMF is derived from the WindSat data and tuned with the aircraft radiometer measurements for very high winds from the Hurricane Ocean Wind Experiment in 1997. The directional signals in the aircraft polarimetric radiometer data are corroborated by coincident Ku-band scatterometer measurements for wind speeds in the range of 20-35 m/s. We applied an iterative retrieval algorithm using the polarimetric brightness temperatures from 18-, 23-, and 37-GHz channels. We find that the root-mean-square direction difference between the Global Data Assimilation System winds and the closest WindSat wind ambiguity is less than 20/spl deg/ for above 7-m/s wind speed. The retrieval analysis supports the consistency of the Windrad05 GMF with the WindSat data.
机译:针对WindSat多频极化微波辐射计,开发了将极化亮度温度的方向响应与海洋表面风相关的地球物理模型函数(GMF)。该GMF源自WindSat数据,并根据1997年飓风“海洋风”实验的极高风,通过飞机辐射计测量进行了调整。飞机极化偏振辐射计数据中的方向信号通过同时进行的Ku波段散射仪测量得到,用于范围为20-35 m / s。我们使用来自18 GHz,23 GHz和37 GHz通道的偏振亮度温度应用了迭代检索算法。我们发现,对于高于7 m / s的风速,全局数据同化系统风与最接近的WindSat风歧义之间的均方根方向差异小于20 / spl deg /。检索分析支持Windrad05 GMF与WindSat数据的一致性。

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