Fig. 5From: Effects of topography and sea surface temperature anomalies on heavy rainfall induced by Typhoon Chaba in 2016Horizontal distribution of accumulated precipitation (mm day−1, shading) in a observation, b CTL, and c CSST. Accumulated rainfall difference (mm day−1, shading) between d CTL and TOPO, e CSST and CSST_TOPO, and f CTL and CSST. The black contour lines in a–f show the height difference (m, contour with 60 m interval) between CTL and TOPO, indicating mountain ranges near Ulsan. The gray dots in a show the locations of observation stationsBack to article page