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. The study of the relationship between water storage andrunoff generation has long been a focus of the hydrological sciences. NASA'sGravity Recovery and Climate Experiment (GRACE) mission provides monthlydepth-integrated information on terrestrial water storage anomalies derivedfrom time-variable gravity observations. As the first basin-scale storagemeasurement technique, these data offer potentially novel insight into thestorage–discharge relationship. Here, we apply GRACE data in a streamflowrecession analysis with river discharge measurements across severalsubdomains of the Mississippi River basin. Nonlinear regression analysiswas used for 12 watersheds to determine that the fraction of baseflow instreams during non-winter months varies from 52 % to 75 % regionally.Additionally, the first quantitative estimate of absolute drainable waterstorage was estimated. For the 2002–2014 period, the drainable storage inthe Mississippi River basin ranged from 2900±400 to 3600±400 km3.

Using GRACE in a streamflow recession to determine drainable water storage in the Mississippi River basin