Fig. 8From: Effects of topography and sea surface temperature anomalies on heavy rainfall induced by Typhoon Chaba in 2016Orographically induced vertical moisture flux (g kg−1 m s−1, shading) of a CTL and b TOPO at \(\eta = 0.955\), computed from the adjacent eta level. The black contour lines indicate the height difference (m, contour with 60 m interval) between CTL and TOPOBack to article page