Simulated Effects of Cropland Expansion on Summer Climate in Eastern China in the Last Three Centuries

<table>Height (color contours) and wind (arrows) at 500 hpa and 750 hpa underlying natural vegetation and the changes induced by land cover conversions from natural vegetation to cropland in 1661, 1820, and 2000.</table>

Advances in Meteorology

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Figure 6

Figure 6: Simulated Effects of Cropland Expansion on Summer Climate in Eastern China in the Last Three Centuries 