Estimation of Risk Thresholds for a Landslide in the Three Gorges Reservoir Based on a KDE-Copula-VaR Approach

<div>Correlations of rapid movement (gray points) with rainfall intensity and reservoir fluctuation. The size of each movement event represents the magnitude of the corresponding event.</div>

Geofluids

fig9

Figure 9

Figure 9: Estimation of Risk Thresholds for a Landslide in the Three Gorges Reservoir Based on a KDE-Copula-VaR Approach 