Figure 12From: Typhoon-induced sea surface cooling during the 2011 and 2012 typhoon seasons: observational evidence and numerical investigations of the sea surface cooling effect using typhoon simulations Differences in equivalent potential temperatures and wind simulated using uncoupled and coupled models. Differences in the 200Â hPa equivalent potential temperatures (color shading) and 500Â hPa wind (vectors) simulated using the uncoupled and coupled models (uncoupled results subtracted from the coupled results) for T1109 at (a) 36Â h, (b) 42Â h, and (c) 60Â h.Back to article page