Research Article
Numerical Simulation of the Direct Radiative Effects of Dust Aerosol on the East Asian Winter Monsoon
Figure 2
Comparison between the NCEP-DOE reanalysis (a, c, e) and Nodust experiment simulated (b, d, f), the SLP (hPa) superimposed on the surface wind (m s−1) (a, b), the 850 hPa wind (c, d), and the 200 hPa U component of wind (e, f), averaged in winter (DJF) during 2000–2009 period. The yellow area in (c, d) represents the topography below 850 hPa altitude.
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