Abstract

© 2015 by the authors. We evaluate performance of the Catchment Land Surface Model under flood conditions after the assimilation of observations of the terrestrial water storage anomaly from NASA's Gravity Recovery and Climate Experiment. Assimilation offers three key benefits for the viability of GRACE observations to operational applications: near-real time analysis; a downscaling of GRACE's coarse spatial resolution; and state disaggregation of the vertically-integrated TWSA. We select the 2011 flood event in the Missouri river basin as a case study, and find that assimilation generally made the model wetter in the months preceding flood. We compare model outputs with observations from 14 USGS groundwater wells to assess improvements after assimilation. Finally, we examine disaggregated water storage information to improve the mechanistic understanding of event generation. Validation establishes that assimilation improved the model skill substantially, increasing regional groundwater anomaly correlation from 0.58 to 0.86. For the 2011 flood event in the Missouri river basin, results show that groundwater and snow water equivalent were contributors to pre-event flood potential, providing spatially-distributed early warning information.