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 the boundary layer at Arou station in June at 12:00: (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 12

Figure 12: Effects of Initial Drivers and Land Use on WRF Modeling for Near-Surface Fields and Atmospheric Boundary Layer over the Northeastern Tibetan Plateau 

Figure 12 | Effects of Initial Drivers and Land Use on WRF Modeling for Near-Surface Fields and Atmospheric Boundary Layer over the Northeastern Tibetan Plateau 