Fig. 5: SSTA-related Pacific circulation, divergence, and OLR anomalies.
From: Interdecadal variability of tropical cyclone intensification rates in the Western North Pacific
Regression maps of a 850 hPa wind with OLR overlay, and b 200 hPa wind with 200 hPa divergence overlay, based on SST anomaly time series from the first SVD mode. Black dots indicate areas where the regression exceeds the 95% significance level.
