The Effect of the Ocean Eddy on Tropical Cyclone Intensity

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The effect of translation speed upon the intensity of tropical cyclones over the tropical ocean (2012, unknown): “The rational behind this effort is that the presence of warm eddies and a deeper than normal mixed layer have been linked to a particularly weak SST cooling under the eye of the TC [e.g., Shay et al. , 2000; Wu et al. , 2007], reducing the negative SST feedback on TC intensity.”
Effects of the Cold Core Eddy on Tropical Cyclone Intensity and Structure under Idealized Air–Sea Interaction Conditions (2013, background): “…serves as an insulator against the negative feedback of the ocean, and thus as a TC encounters a WCE, the SST cooling is significantly reduced and the storm rapid intensification always occurs (Hong et al. 2000; Lin et al. 2005; McTaggart-Cowan et al. 2007; Wu et al. 2007; Jaimes and Shay 2009).”
Upper-Ocean Thermal Structure and the Western North Pacific Category 5 Typhoons. Part II: Dependence on Translation Speed (2009, unknown): “the ocean surface, but also with the entire upper-ocean column (typically from surface down to 100–200 m; Perlroth 1967; Leipper and Volgenau 1972; Gray 1979; Holliday and Thompson 1979; Shay et al. 2000; Cione and Uhlhorn 2003; Goni and Trinanes 2003; Lin et al. 2005, 2008, 2009; Pun et al. 2007; W”