Figures & data
Table 1. Specification of ensemble simulations for both historical (present) and future (+4K) runs.
Figure 1. TC tracks around Tokyo Bay (200 km × 200 km scale) by (a) single ensemble and (b) 1,000 ensemble simulation.
![Figure 1. TC tracks around Tokyo Bay (200 km × 200 km scale) by (a) single ensemble and (b) 1,000 ensemble simulation.](/cms/asset/a58b8dd1-efba-4861-a8e0-d5e24d2e0820/tcej_a_1586290_f0001_oc.jpg)
Figure 3. Non-exceedance probability of minimum central pressure Pmin for (a) global and (b) WNP (blue line: historical climate, red line: future climate (+4K), black line: observation by IBTrACS, shade: 95% confidence interval).
![Figure 3. Non-exceedance probability of minimum central pressure Pmin for (a) global and (b) WNP (blue line: historical climate, red line: future climate (+4K), black line: observation by IBTrACS, shade: 95% confidence interval).](/cms/asset/8c68fdd1-9118-4435-a67c-84a8c3edc644/tcej_a_1586290_f0003_oc.jpg)
Figure 4. Probability density function of annual cyclogenesis number over (a) global and in (b) WNP (blue solid line: historical climate with 100 ensemble runs, blue dashed line: historical climate with 1 ensemble run, red solid line: future climate (+4K) with 90 ensemble runs, red dashed line: future climate (+4K) with 1 ensemble run, black line: observed (IBTrACS), shade: 95% confidence interval).
![Figure 4. Probability density function of annual cyclogenesis number over (a) global and in (b) WNP (blue solid line: historical climate with 100 ensemble runs, blue dashed line: historical climate with 1 ensemble run, red solid line: future climate (+4K) with 90 ensemble runs, red dashed line: future climate (+4K) with 1 ensemble run, black line: observed (IBTrACS), shade: 95% confidence interval).](/cms/asset/0942ae18-b577-483a-9448-96d1dbc9ad16/tcej_a_1586290_f0004_oc.jpg)
Figure 5. Future changes of centroids of TCs (upward triangle: cyclogenesis, circle: most developed, downward triangle: cyclolysis, blue: historical climate, red: future climate (+4K)). Changes are magnified by factor of 3.
![Figure 5. Future changes of centroids of TCs (upward triangle: cyclogenesis, circle: most developed, downward triangle: cyclolysis, blue: historical climate, red: future climate (+4K)). Changes are magnified by factor of 3.](/cms/asset/915609f1-44c0-41e0-9c10-76429a08cf38/tcej_a_1586290_f0005_oc.jpg)
Figure 6. Future change in extreme distribution of storm surge height in Osaka Bay and Tokyo Bay, Japan. (Blue line: historical climate, red libne: future climate (+4K), thick colored line: empirical non-exceedance probability function, thin colored line: smoothed function).
![Figure 6. Future change in extreme distribution of storm surge height in Osaka Bay and Tokyo Bay, Japan. (Blue line: historical climate, red libne: future climate (+4K), thick colored line: empirical non-exceedance probability function, thin colored line: smoothed function).](/cms/asset/d5c82ec1-6894-493b-9452-042ea7976f61/tcej_a_1586290_f0006_oc.jpg)
Figure 7. Future change components in extreme distribution of storm surge height in Osaka Bay, Japan. (Thick black line: total change of surge height, red solid line: change due to frequency, blue solid: change due to intensity and track shifts, green line: residual).
![Figure 7. Future change components in extreme distribution of storm surge height in Osaka Bay, Japan. (Thick black line: total change of surge height, red solid line: change due to frequency, blue solid: change due to intensity and track shifts, green line: residual).](/cms/asset/28e1a412-0622-4fbd-a368-8bc58e2a5857/tcej_a_1586290_f0007_oc.jpg)
Figure 8. Comparison of 100-year return value of global extreme sea level along the coast derived from (a) reanalysis data (GTSR; Muis et al., 2016) and (b) this study. The value at each location is normalized by the global maximum value (unit: ratio).
![Figure 8. Comparison of 100-year return value of global extreme sea level along the coast derived from (a) reanalysis data (GTSR; Muis et al., 2016) and (b) this study. The value at each location is normalized by the global maximum value (unit: ratio).](/cms/asset/5ebf47c8-9cb6-4d63-b56c-4d7e2efa805d/tcej_a_1586290_f0008_oc.jpg)