Fig. 11From: Effects of topography and sea surface temperature anomalies on heavy rainfall induced by Typhoon Chaba in 2016Horizontal distribution of 850 hPa water vapor (g kg−1) in a CTL and b CSST at 0000 UTC on October 5, and c time series of difference in water vapor (g kg−1) and precipitable water (kg m−2) between CTL and CSST within the blue box in the a, bBack to article page