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

Figure 6

Dust mixing ratio changes at 600 hPa (μg kg⁻¹) between different numerical experiments in spring (a, c, e) and summer (b, d, f): (a, b) ; (c, d) ; (e, f) () minus ().

(a)

(b)

(c)

(d)

(e)

(f)