Fig. 10From: Effects of topography and sea surface temperature anomalies on heavy rainfall induced by Typhoon Chaba in 2016Vertical structures of simulated typhoon at 1200 UTC on October 4. Horizontal wind (shading, m s−1) and potential temperature (contour, K with 5 K interval) in a CTL and b CSST, tangential wind (m s−1) in c CTL and d CSST, and radial wind (m s−1) in e CTL and f CSSTBack to article page