Fig. 1From: 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 areas covered in the present numerical simulation. The computational areas for a the 9 km grid domain (D01), the 3 km grid domain (D02), and 1 km grid domain (D03) and b the 200 m grid domains (D04) nested in D03Back to article page