“…Compared to IR, MW provides more direct and accurate precipitation measurements because of its sensitivity to rain/ice particles, whereas IRâbased algorithms are often built on empirical and indirect links between cloud top brightness temperature ( T b ) and surface precipitation (Huffman et al, ; Kidd et al, ; Sorooshian et al, ). Active microwave sensors, that is, spaceborne radars, often provide more direct and accurate precipitation estimates than passive microwave (PMW) sensors (Behrangi et al, ; Gao et al, ; Tang et al, ; Tang, Long, et al, ). So far, there have been three popular spaceborne radars for observing precipitation, that is, the Kuâband precipitation radar onboard the Tropical Rainfall Measuring Mission (TRMM) satellite operating from 1997 to 2015, the Wâband Cloud Profiling Radar (CPR) onboard the CloudSat operating from 2006 to the present, and the Dualâfrequency Precipitation Radar (DPR) onboard the Global Precipitation Measurement (GPM) Core Observatory operating from 2014 to the present.…”