The Observed State of the Water Cycle in the Early Twenty-First Century

By Matthew Rodell, Hiroko K. Beaudoing, Tristan L'Ecuyer, W. Olson, James S. Famiglietti, Paul R. Houser, Robert F. Adler, M. Bosilovich, C. Clayson, D. Chambers and 12 more. 2015

257 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/96ed915fcc05d134f11b1eece0cf5b0e0a41424f

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In Global and Planetary Change

1. G. Sposito

Citations in the corpus

• Understanding the budyko equation (2017, methodology): “Indirect measurement using combinations of ground-based, satellite-based, and model-based methods is therefore the usual approach for determining evapotranspiration at catchment to global scales [2].”
• The DOE E3SM Coupled Model Version 1: Description and Results at High Resolution (2019, unknown): “Thus, while E3SMv1 global-average precipitation is larger than the Rodell et al. (2015) estimate used in Table 5 and the GPCP estimate used in Figure 10, it is within uncertainty bounds for Stephens et al. (2012) and Wild et al. (2012).”
• Evaluating the Hydrological Cycle over Land Using the Newly-Corrected Precipitation Climatology from the Global Precipitation Climatology Centre (GPCC) (2017, background): “Average water transport/exchanges in km3 per year as derived from GPCC’s precipitation climatology for 1951–2000 land surface precipitation, numbers for precipitation over oceans, evapotranspiration/evaporation over land/ocean taken from [13,14], background picture by courtesy of A.”