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

<table>Changes in surface downward solar radiation, reflected shortwave radiation at the surface, surface sensible heat flux, and latent heat flux induced by land cover conversions from natural vegetation to cropland in 1661, 1820, and 2000.</table>

Advances in Meteorology

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Figure 5

Figure 5: Simulated Effects of Cropland Expansion on Summer Climate in Eastern China in the Last Three Centuries 