Research Article
Numerical Modeling of Topography-Modulated Dust Aerosol Distribution and Its Influence on the Onset of East Asian Summer Monsoon
Figure 3
Observed (a, c) and simulated (b, d) mean precipitation rate (units: mm day−1) and 850 hPa wind (units: m s−1) in spring (a, b) and summer (c, d). The black lines are the terrain contours of 2000 m.
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