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Shruti A. Upadhyaya, Pierre-Emmanuel Kirstetter, Jonathan J. Gourley, and Robert J. Kuligowski

resolutions are critical for near-real-time applications such as rapid monitoring and forecasting of high-impact societal events like flash floods, debris flows, and shallow landslides. Such resolution can be obtained primarily from satellite sensors on board geostationary Earth orbit (GEO) platforms. NOAA’s Advanced Baseline Imager (ABI) sensor on board the latest generation of Geostationary Operational Environmental Satellites (GOES-R Series) provides 3 times more spectral channels, 4 times the

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Clément Guilloteau and Efi Foufoula-Georgiou

. 1996 , 2001 , 2015 ; Kubota et al. 2007 ; Gopalan et al. 2010 ; Mugnai et al. 2013 ; Ebtehaj et al. 2015 ; Kidd et al. 2016 ; Petković et al. 2018 ). The TRMM ( Kummerow et al. 2000 ) and GPM ( Hou et al. 2014 ; Skofronick-Jackson et al. 2017 ) satellite missions in particular provided the data and the research framework allowing the successful development of research and operational retrieval algorithms. Today, the GPM Microwave Imager (GMI) is integrated in an international constellation

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Clement Guilloteau, Efi Foufoula-Georgiou, Pierre Kirstetter, Jackson Tan, and George J. Huffman

Conference , B. Webb et al., Eds., British Hydrological Society, 120–127. Habib , E. , W. F. Krajewski , and A. Kruger , 2001 : Sampling errors of tipping-bucket rain gauge measurements . J. Hydrol. Eng. , 6 , 159 – 166 , https://doi.org/10.1061/(ASCE)1084-0699(2001)6:2(159) . 10.1061/(ASCE)1084-0699(2001)6:2(159) Harris , D. , E. Foufoula-Georgiou , K. K. Droegemeier , and J. J. Levit , 2001 : Multiscale statistical properties of a high-resolution precipitation forecast . J

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Chandra Rupa Rajulapati, Simon Michael Papalexiou, Martyn P. Clark, Saman Razavi, Guoqiang Tang, and John W. Pomeroy

Forecast System Reanalysis (CFSR) v2, and 5) Water and Global Change (WATCH) Forcing Data–ERA-Interim (WFDEI) version 14 August 2018. The PERSN-CDR, MSWEP, and WFDEI datasets combine information from observations, satellites, and reanalysis. The CPC uses only observations and the CFSR is purely a reanalysis product. PERSN-CDR is derived from the satellite data (Gridsat-B1), adjusted using the precipitation data from Global Precipitation Climatology Project ( Ashouri et al. 2015 ; Nguyen et al. 2018

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