Climate and Catastrophe Risk Assessment - Asia slide image

Climate and Catastrophe Risk Assessment - Asia

Difference (m/s) Difference (hPa) Met Office cass Data Resolution 2 1.0 0.5. 0.0- (a) Gust Speed (1hr max) -0.5 -1.0 1001 75 50 45 25 0 (b) MSLP (1hr min) 15 10 20 30 40 50 60 70 80 90 95 99 1.5km percentiles www.metoffice.gov.uk Federal Ministry for the Environment, Nature Conservation and Nuclear Safety part of the Oasis Platform for Climate and Catastrophe Risk Assessment - Asia, a project funded by the International Climate Initiative (IKI) 1.5km faster 1.5km slower All subsequent analysis presented here focuses on 4.4km data - mainly for computational reasons (further discussion of this later). But we also examine the difference between the two resolutions for two key variables: maximum gust speed and minimum mean sea-level pressure. Differences in maximum gust speed footprints, for the 1st to 80th Key Point (c) ► percentiles, of the 1.5km data are roughly O(0.5 m/s) faster than the 4.4km data. For the very highest gust speeds (90th, 95th and 99th percentiles of the 1.5km data) the differences with the 4.4km data shows much greater variability. We suspect that the minimal difference seen in the upper extreme percentiles results from under sampling rather than a systematic difference. 1.5km shallower 1.5km deeper Key Point (d) ▼ For minimum MSLP footprints, extreme lows of the 1.5km data are [50, 87] hPa and [10, 37] hPa shallower for the 1st and 5th percentiles respectively (90% HDI). Given the relationship between central pressure deficit (i.e. the difference between the tropical cyclone central pressure and the environmental pressure outside the tropical cyclone), peak wind speed and tropical cyclone size, this comparisons suggests that 1.5km storms must also be smaller in size than the 4.4km storms. Key Point (e) ▲ 7 B CC BY
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