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Vinodkumar, A. Chandrasekar, K. Alapaty, and Dev Niyogi

. Also, FASDAS ensures soil moisture adjustment so that errors are reduced in the surface layer simulation. The inverse method also introduces observed temporal variability in the deep soil moisture on a weekly-to-monthly time scale. Childs et al. (2006) numerically simulated the convective initiation over the southern Great Plains of the United States during the International H 2 O Project 2002 (IHOP_2002) using the fifth-generation Pennsylvania State University–National Center for Atmospheric

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