Fig. 10.From: Volume change of the magma reservoir relating to the 2011 Kirishima Shinmoe-dake eruption—Charging, discharging and recharging process inferred from GPS measurementsTrade-offs between estimated source parameters for the period after the climax event. The open double circle shows the best fit model. Dots indicate estimates of bootstrap tests. Estimated source volume and depth have a strong trade-off, while other parameters show little correlation.Back to article page