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Progress in Earth and Planetary Science
Fig. 2 | Progress in Earth and Planetary Science

Fig. 2

From: Benefits of high-resolution downscaling experiments for assessing strong wind hazard at local scales in complex terrain: a case study of Typhoon Songda (2004)

Fig. 2

Comparison of the surface winds simulated in D03 with the observations at surface stations. a The difference of the temporally averaged wind speed from the simulation to the observation. b The ratio of the variance of the simulation wind speed against that of the observation. c The Spearman’s rank correlation coefficient of the temporal change of wind speed between the simulation and the observation. The color shading in all the panels indicates the ground elevation (m)

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