Tropical Cyclone Intensity Change from a Simple Ocean–Atmosphere Coupled Model

By J. Chan, Y. Duan, L. Shay. 2001

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Effects of Tropical Cyclones on Ocean Heat Transport in a High-Resolution Coupled General Circulation Model (2011, background): “The sea surface temperature (SST) feedback generally leads to a weakening of the cyclone intensity due to the reduction of the total heat flux into the atmosphere (Schade and Emanuel 1999; Chan et al. 2001).”
Effects of the Cold Core Eddy on Tropical Cyclone Intensity and Structure under Idealized Air–Sea Interaction Conditions (2013, background): “…atmosphere– ocean coupled models further clarified the negative effects of ocean response on TC development in detail by considering more realistic and complex coupling processes (e.g., Bender et al. 1993; Bender and Ginis 2000; Chan et al. 2001; Zhu et al. 2004; Chen et al. 2010).”
The Effect of the Ocean Eddy on Tropical Cyclone Intensity (2007, background): “This negative feedback to the TC intensity is clearly a function of the oceanic thermal conditions (Bender et al. 1993; Schade and Emanuel 1999; Hong et al. 2000; Shay et al. 2000; Bender and Ginis 2000; Chan et al. 2001; Lin et al. 2005).”