Hydrological Variability in the Arid Region of Northwest China from 2002 to 2013

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/amete/volume-2018/1502472/figures/1502472.fig.008a.svgz" name="1502472.fig.008a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Hexi-Alashan</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/amete/volume-2018/1502472/figures/1502472.fig.008b.svgz" name="1502472.fig.008b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Northern Xinjiang</td></tr><tr class="fig-image" id="c"><td><object data="https://static.hindawi.com/articles/amete/volume-2018/1502472/figures/1502472.fig.008c.svgz" name="1502472.fig.008c" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(c) </b>Southern Xinjiang</td></tr></table>

<div>Multiple-year averaged monthly variations of TWSA and its components (SMA, SWEA, and inverse GSWA) as well as precipitation in the three subregions.</div>

Advances in Meteorology

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Figure 8

Figure 8: Hydrological Variability in the Arid Region of Northwest China from 2002 to 2013 