被动微波交叉航迹测深仪降水反演

C. Kidd, S. Ringerud, G. Skofronick-Jackson, G. Huffman
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引用次数: 1

摘要

降水(雨雪)是一个关键的地球物理参数。由于时间和空间的可变性,利用所有可用的数据源,特别是所有可用的无源微波传感器至关重要。本文重点研究了一种物理检索方案的发展,以获得来自交叉轨迹无源微波传感器的降水估计。“雷霆”)。对地球入射角变化对反演结果影响的初步研究表明,虽然极化变化很小,但分辨率起了更大的作用。虽然最初设想的方案是利用卫星/地面观测产生的75个扫描位置/地面型数据库,但最后方案利用具有单一数据库的模型生成数据库;给出了该方案的结果。最后介绍了对下一代交叉航迹检索方案的初步研究工作。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Precipitation retrievals from passive microwave cross-track sounding instruments
Precipitation (rain and snow) is a key geophysical parameter. Due the temporal and spatial variability it is vital to exploit all available data sources, and in particular all available passive microwave sensors. This paper concentrates upon the development of a physical retrieval scheme to obtain precipitation estimates from cross-track passive microwave sensors (a.k.a. `sounders'). Initial studies into the impact of the variable Earth incidence angle upon the retrievals suggested that while changes in polarization were minimal, resolution played a greater part. Although the scheme was originally envisaged with 75 scan-position/surface type databases generated from satellite/surface observations, the final scheme utilizes a model-generated database with a single database; results from this scheme are presented. The paper finally presents some initial work from investigations into the next-generated cross-track retrieval schemes.
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