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

Figure 6

The profiles of the 10-year summer mean differences between BATS and CLM for (a) zonal wind , (b) meridional wind , (c) air temperature , (d) vertical velocity , (e) geopotential height , (f) water vapor mixing ratio , and (g) relative humility RH over the TP.

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(b)

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