Variations of Near Surface Energy Balance Caused by Land Cover Changes in the Semiarid Grassland Area of China

<table class="table-group" width="800px"><tr class="fig-image" id="a"><td><img alt="894147.fig.004a" src="https://static.hindawi.com/articles/amete/volume-2014/894147/figures/894147.fig.004a.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(a) </b>REG scenario in 2030</td></tr></table></td></tr><tr class="fig-image" id="b"><td><img alt="894147.fig.004b" src="https://static.hindawi.com/articles/amete/volume-2014/894147/figures/894147.fig.004b.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(b) </b>CES scenario in 2030</td></tr></table></td></tr><tr class="fig-image" id="c"><td><img alt="894147.fig.004c" src="https://static.hindawi.com/articles/amete/volume-2014/894147/figures/894147.fig.004c.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(c) </b>REG scenario in 2050</td></tr></table></td></tr><tr class="fig-image" id="d"><td><img alt="894147.fig.004d" src="https://static.hindawi.com/articles/amete/volume-2014/894147/figures/894147.fig.004d.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(d) </b>CES scenario in 2050</td></tr></table></td></tr></table>

<table>Latent heat flux changes under different scenarios in 2030 and 2050 in the semiarid grassland area of China (unit: W/m<sup>2</sup>).</table>

Advances in Meteorology

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Figure 4

Figure 4: Variations of Near Surface Energy Balance Caused by Land Cover Changes in the Semiarid Grassland Area of China 