Warming of SST in the cool wake of a moving hurricane

By J. Price, J. Morzel, P. Niiler. 2008

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Parameterization of mixed layer eddies. III: Implementation and impact in global ocean climate simulations (2010, background): “, hurricanes) combined with large-scale strain may also lead to horizontal density gradients (e.g., Price, 1981; Ferrari and Rudnick, 2000; D’Asaro et al., 2007; Price et al., 2008).”
Effects of the Cold Core Eddy on Tropical Cyclone Intensity and Structure under Idealized Air–Sea Interaction Conditions (2013, background): “…the cold wake are mainly determined by the temperature profile in the upper ocean and the TC translation speed, and the right bias of the cold wake is primarily due to the asymmetric turning of wind stress arisen from the translation of a vortical wind pattern (Price 1981; Price et al. 1994, 2008).”