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Progress in Earth and Planetary Science
Fig. 6 | Progress in Earth and Planetary Science

Fig. 6

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. 6

Relationships between terrain slope and mean wind speed in the analysis areas. Relationships of the temporal mean wind speeds against the terrain slope angle for the 1 km grid case (black dots) and the 200 m grid case (gray dots) in the area (a) A, (b) B, and (c) C. Red solid and dotted lines indicate the linear regression line for the 200 m grid and the 1 km grid case, respectively

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