Effects of Initial Drivers and Land Use on WRF Modeling for Near-Surface Fields and Atmospheric Boundary Layer over the Northeastern Tibetan Plateau

<div>Average vertical profile of boundary layer at Arou station in June at 0:00: (a) potential temperature, (b) water vapor mixing ratio, (c) U wind speed, and (d) V wind speed.</div>

Advances in Meteorology

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Figure 13

Figure 13: Effects of Initial Drivers and Land Use on WRF Modeling for Near-Surface Fields and Atmospheric Boundary Layer over the Northeastern Tibetan Plateau 

Figure 13 | Effects of Initial Drivers and Land Use on WRF Modeling for Near-Surface Fields and Atmospheric Boundary Layer over the Northeastern Tibetan Plateau 