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

transition regions that involve diverse processes such as the coastal interface between land and ocean. A detailed understanding and observation of precipitation over the land–coast–ocean continuum is still lacking, especially since observations over oceans are limited by remoteness and scale. Observations of precipitation over the ocean can be conducted by using weather radars situated on islands and coastlines and with rain gauges on ships and buoy gauge arrays (e.g., Anagnostou et al. 1999 ; Smith

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Andrea Camplani, Daniele Casella, Paolo Sanò, and Giulia Panegrossi

available only over CONUS, all the results based on this dataset are valid at a regional scale. While all sun synchronous GMI orbits over CONUS have been considered, only ATMS ascending orbits (between 0600 and 1300 UTC), closest in time to the SNODAS reference time (0600 UTC), have been selected. The dataset has been built following the same procedures used for the development and validation datasets, obtaining a snow-cover occurrence index, a land fraction index (since SNODAS provides information only

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

1. Introduction Satellite-derived quantitative precipitation estimation (QPE) products have been around for several decades and are now commonly used in climate studies ( Mehta and Yang 2008 ; Roca et al. 2014 ; Kerns and Chen 2020 ), hydrologic modeling and prediction ( Casse and Gosset 2015 ), and various other applications ( Kirschbaum et al. 2017 ), including vegetation monitoring ( Hilker et al. 2014 ; Suepa et al. 2016 ), landslide risk management ( Kirschbaum and Stanley 2018

Open access