Numerical Modeling of Topography-Modulated Dust Aerosol Distribution and Its Influence on the Onset of East Asian Summer Monsoon

<div>Comparison between RegCM4.1 simulated and CRU observed annual cycles of monthly precipitation (mm/day) regional averaged for the north China (a) (38°–42°N, 110°–120°E) and south China (25°–30°N, 110°–115°E).</div>

Advances in Meteorology

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Figure 4

Figure 4: Numerical Modeling of Topography-Modulated Dust Aerosol Distribution and Its Influence on the Onset of East Asian Summer Monsoon 