Influences of Two Land-Surface Schemes on RegCM4 Precipitation Simulations over the Tibetan Plateau

<div>The summer mean wind (units: m/s) and temperature (units: °C) distributions at 500 hPa (a) and 200 hPa (b) over the TP during 1992–2001. (A) and (D) represent ERA40; (B) and (E) represent BATS; and (C) and (F) represent CLM.</div>

Advances in Meteorology

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Figure 5

Figure 5: Influences of Two Land-Surface Schemes on RegCM4 Precipitation Simulations over the Tibetan Plateau 