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Official Journal of the Asia Oceania Geosciences Society (AOGS)

Fig. 5 | Geoscience Letters

Fig. 5

From: Effects of topography and sea surface temperature anomalies on heavy rainfall induced by Typhoon Chaba in 2016

Fig. 5

Horizontal 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 af 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 stations

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