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Di Wu, Christa Peters-Lidard, Wei-Kuo Tao, and Walter Petersen

. 2008 ; Seity et al. 2011 ; Baldauf et al. 2011 ). The positive feedback between soil moisture and precipitation is also well known. The wet soil surface facilitates heat and moisture transport into the planetary boundary layer (PBL), so the moistening of lower PBL is likely to produce localized convective precipitation. Gallus and Segal (2000) found that precipitation amounts respond to the change of soil moisture differently among runs with different convective parameterizations. Case et al

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