Research Article
Numerical Simulation of the Direct Radiative Effects of Dust Aerosol on the East Asian Winter Monsoon
Figure 10
Precipitation rate for (a) Nodust, (b) Dust, (c) CRU, and (d) percentage change between Dust and Nodust experiments averaged in winter during 2000–2009 period; the black dots in (d) indicate areas in which the difference is statistically significant at the 95% confidence level (Student’s t-test).
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