Michael Barlage, Fei Chen, Roy Rasmussen, Zhe Zhang, Gonzalo Miguez-Macho

DOI: https://doi.org/10.1029/2020GL092171

Abstract
This study explores the impacts of groundwater processes on the simulated land-surface water balance and hydrometeorology. Observations are compared to multiscale Weather Research and Forecasting (WRF) simulations of three summer seasons: 2012, 2013, and 2014. Results show that a grid spacing of 3 km or smaller is necessary to capture small-scale river and stream networks and associated shallow water tables, which supplies additional root-zone water double that of simulations with 9-km and 27-km grid spacing and is critical to replenishing the depleted vegetation root zones and leads to 150 mm more evapotranspiration. Including groundwater processes in convection-permitting models is effective to reduce: (1) 2-m temperature warm biases from 5–6 to 2–3 °C and (2) the low precipitation bias by half. The additional groundwater supply to active soil flux in convection-permitting simulations with groundwater for June-August is nearly translated into the same amount of increased precipitation in the domain investigated.