Influences of Two Land-Surface Schemes on RegCM4 Precipitation Simulations over the Tibetan Plateau
(a) The summer surface soil moisture difference between the BATS and CLM experiments (units: ). (b) The same as (a) but for evapotranspiration (ET) (units: mm). (c) The same as (a) but for sensible heat flux (SHF) (units: ). (d) The same as (a) but for 2 m air temperature (units: °C) during 1992–2001.