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Nicholas A. Bond, Meghan F. Cronin, and Matthew Garvert

sensible and latent heat, which themselves represent the primary energy source for tropical cyclones (e.g., Emanuel 1986 ). One might expect that anomalously warm SSTs would tend to be associated with delayed transitions for storms moving poleward, and that cold SSTs would be associated with hastened transitions, all other factors being equal. Thus, the effects of the regional SST on these storms may not have just local manifestations. Modifications in storm properties have potential impacts on the

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