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Accounting for surface ice and snow in the goddard profiling algorithm rain rate retrievals

机译:在戈达德剖析算法降雨率检索中考虑表层冰雪

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A recurring challenge for microwave precipitation retrieval algorithms is the separation of precipitation from surface snow. Cold surfaces can have similar radiometric characteristics to suspended precipitation particles, such that surface snow reduces the detection accuracy of precipitation algorithms. Snow detection is typically performed using a collection of heritage algorithms, however surface snow can often go undetected and lead to erroneous precipitation retrievals. This study examines flagging procedures in the Goddard Profiling Algorithm 2010 V2 as it applies to the Advanced Scanning Microwave Radiometer 2 over the United States in the winter of 2014-2015. The legacy algorithms are often not reliable, such that a climatological screen is applied in known snowy regions. The diurnal cycle of brightness temperatures also complicates resolving rain when using the static legacy algorithms.
机译:微波降水检索算法的一个反复出现的挑战是将降水与地表雪分离。冷表面可能具有与悬浮的沉淀颗粒相似的辐射特征,因此,表面积雪会降低沉淀算法的检测精度。积雪检测通常使用一系列传统算法进行,但是地表积雪经常无法被检测到,并导致错误的降水获取。这项研究研究了戈达德剖析算法2010 V2中的标记程序,因为该程序适用于2014-2015年冬季美国全境的Advanced Scanning Microwave Radiometer 2。传统算法通常不可靠,因此在已知的多雪区域中应用了气候屏蔽。使用静态传统算法时,亮度温度的昼夜循环还会使下雨变得更加复杂。

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