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.hindawi.com/articles/geofluids/volume-2018/8126518/figures/8126518.fig.006a.svgz" name="8126518.fig.006a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Southern region</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2018/8126518/figures/8126518.fig.006b.svgz" name="8126518.fig.006b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Northern region</td></tr></table>

<div>The lower boundaries of rainfall condition for triggering landslides in 2006–2008 and 2010–2014. (a) 58 landslides in the southern region. The numbers labeled around the data lower than the lower boundary of 06–08 mean the occurrence year of event. (b) 35 landslides in the northern region.</div>

Geofluids

fig6

Figure 6

Figure 6: Impact of an Extreme Typhoon Event on Subsequent Sediment Discharges and Rainfall-Driven Landslides in Affected Mountainous Regions of Taiwan 

Figure 6 | Impact of an Extreme Typhoon Event on Subsequent Sediment Discharges and Rainfall-Driven Landslides in Affected Mountainous Regions of Taiwan 