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Typhoon Francisco (2013) experienced unusually rapid weakening (RW) with its maximum surface wind decreasing by 45 kt (1 kt ≈ 0.51 m s −1 ) over 24 h as measured from the satellite-derived advanced Dvorak technique (ADT) dataset, which is more than twice the weakening rate defined as RW by DeMaria. The mechanisms leading to the extreme RW event of Francisco are examined based on observational analysis and simulations by coupling the Weather Research and Forecasting (WRF) Model, version 3.7, with the Stony Brook Parallel Ocean Model (sbPOM). The RW of Francisco took place in a relatively favorable atmospheric environment while passing over detrimental oceanic conditions, dominated by the presence of a cold-core eddy. The passages of two prior typhoons apparently intensified the cold-core eddy, contributing to a major role of eddy feedback on RW for Francisco. The structural changes in Francisco accompanying eddy interaction are characterized by a substantially enlarged eye size, which evolved from ~20 to ~100 km in diameter, as indicated from satellite images. Numerical simulations suggest that the eddy is prominent in weakening the intensity of Francisco during the storm–eddy interaction, with its role less significant but still comparable to that of the cold wake. Both the cooler water and stronger upward motion in the eddy lead to a larger sea surface temperature decrease induced by Francisco, which results in a nearly 50% decrease of surface enthalpy flux, suppressed convective bursts, and a 50% reduction in latent heat release. These results underscore the potential importance of open-ocean, cold-core eddies in contributing to the RW of tropical cyclones.

A Study of the Interaction between Typhoon Francisco (2013) and a Cold-Core Eddy. Part I: Rapid Weakening