While gauge observations serve as a traditional way to measure precipitation, remote sensing technology has grown rapidly in recent decades and become another effective method for estimating precipitation (Kucera et al., 2013; Yang et al., 2013). By detecting the properties of precipitating clouds, satellites estimate snapshots of the precipitation rate from infrared (IR) sensors, relatively direct passive microwave (PMW) sensors, or Precipitation Radar (PR) (Kummerow et al., 2015; Sun et al., 2018; Yang et al., 2013). By further combining these multiple satellite sources, quasi-global gridded products have been developed (e.g., Tropical Rainfall Measuring Mission (TRMM) Multisatellite Precipitation Analysis (TMPA), Climate Prediction Center (CPC) Morphing (CMORPH), Precipitation Estimation from Remotely Sensed Information using Artificial Neural Networks (PERSIANN), and Integrated MultisatellitE Retrievals for Global Precipitation Measurement (GPM) (IMERG)), which have been used in a wide range of applications (