Impact of an Extreme Typhoon Event on Subsequent Sediment Discharges and Rainfall-Driven Landslides in Affected Mountainous Regions of Taiwan

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static-preview.hindawi.com/articles/geofluids/volume-2018/8126518/figures/8126518.fig.003a.svgz" name="8126518.fig.003a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Zhuoshui River (1510H057)</td></tr><tr class="fig-image" id="b"><td><object data="https://static-preview.hindawi.com/articles/geofluids/volume-2018/8126518/figures/8126518.fig.003b.svgz" name="8126518.fig.003b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Zengwen River (1630H019)</td></tr><tr class="fig-image" id="c"><td><object data="https://static-preview.hindawi.com/articles/geofluids/volume-2018/8126518/figures/8126518.fig.003c.svgz" name="8126518.fig.003c" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(c) </b>Gaoping River (1730H043)</td></tr></table>

<div>Cumulative water flux and SSD in (a) the Zhuoshui River, (b) the Zengwen River, and (c) the Gaoping River in the period from 1997 to 2016.</div>

Geofluids

fig3

Figure 3

Figure 3: Impact of an Extreme Typhoon Event on Subsequent Sediment Discharges and Rainfall-Driven Landslides in Affected Mountainous Regions of Taiwan 

Figure 3 | Impact of an Extreme Typhoon Event on Subsequent Sediment Discharges and Rainfall-Driven Landslides in Affected Mountainous Regions of Taiwan 