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  • Global Precipitation Measurement (GPM): Science and Applications x
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Stephen E. Lang and Wei-Kuo Tao

Syst. , 8 , 66 – 95 , https://doi.org/10.1002/2015MS000469 . 10.1002/2015MS000469 Chong , M. , and D. Hauser , 1990 : A tropical squall line observed during the COPT 81 experiment in West Africa. Part III: Heat and moisture budgets . Mon. Wea. Rev. , 118 , 1696 – 1706 , https://doi.org/10.1175/1520-0493(1990)118<1696:ATSLOD>2.0.CO;2 . 10.1175/1520-0493(1990)118<1696:ATSLOD>2.0.CO;2 Choudhury , A. D. , and R. Krishnan , 2011 : Dynamical response of the South Asian monsoon trough

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Yagmur Derin, Pierre-Emmanuel Kirstetter, and Jonathan J. Gourley

snow and ice properties ( Takbiri et al. 2019 ; Kummerow 2020 ). Over the ocean, PMW algorithms can separate the surface radiation signal from the emission signal for liquid hydrometeors. Over land, microwave emissivity is sensitive to soil moisture, particularly at lower frequencies, which obscures the liquid hydrometeor emission signals. Hence, coastal areas present high emissivity gradients that challenge GPROF2017 precipitation retrieval. These retrievals are then intercalibrated to CORRA (the

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