Coupling Analysis of Hydrometeorology and Erosive Landforms Evolution in Loess Plateau, China

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/amete/volume-2016/9732864/figures/9732864.fig.004a.svgz" name="9732864.fig.004a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Erosive precipitation frequency</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/amete/volume-2016/9732864/figures/9732864.fig.004b.svgz" name="9732864.fig.004b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Rainstorm frequency</td></tr><tr class="fig-image" id="c"><td><object data="https://static.hindawi.com/articles/amete/volume-2016/9732864/figures/9732864.fig.004c.svgz" name="9732864.fig.004c" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(c) </b>Heavy rainstorm frequency</td></tr></table>

<div>Frequency of different rainfall types ((a) erosive precipitation, (b) rainstorm, and (c) heavy rainstorm).</div>

Advances in Meteorology

fig4

Figure 4

Figure 4: Coupling Analysis of Hydrometeorology and Erosive Landforms Evolution in Loess Plateau, China 