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Official Journal of the Asia Oceania Geosciences Society (AOGS)

Fig. 4 | Geoscience Letters

Fig. 4

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

Fig. 4

Simulated a track, b minimum sea level pressure (hPa), and c maximum wind speed (m s−1) in the CTL (red), CSST (blue), and JTWC best track data (black) of Typhoon Chaba. The green lines in a indicate the warm SST area as seen in Fig. 3b. The track data of JTWC, CTL, and CSST is 6-hourly tracked data, and time/date is shown along typhoon tracks. Tracking starts at 0000 UTC on October 2 and ends at 0600 UTC on October 5

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