Fig. 5From: Benefits of high-resolution downscaling experiments for assessing strong wind hazard at local scales in complex terrain: a case study of Typhoon Songda (2004)The frequency distribution of the maximum surface wind speeds in the analysis areas. The relative frequency distribution (in %) of the maximum wind speeds during the simulated time period at the grid points in the area (a) A, (b) B, and (c) C for (left) the 1 km grid case and (right) the 200 m grid caseBack to article page