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the “atypical” RI path in sustained, moderate vertical wind shear. We must stress that this cursory climatological inspection is not meant to imply that all TCs in this regime will undergo RI, as both Rios-Berrios and Torn (2017) and Finocchio and Majumdar (2017) demonstrated in a climatological way. Nor do all EPAC TCs undergo this process since the TC has to respond accordingly to the forcing, and this behavior is not exclusive to this basin. From a climatological perspective, it is simply
the “atypical” RI path in sustained, moderate vertical wind shear. We must stress that this cursory climatological inspection is not meant to imply that all TCs in this regime will undergo RI, as both Rios-Berrios and Torn (2017) and Finocchio and Majumdar (2017) demonstrated in a climatological way. Nor do all EPAC TCs undergo this process since the TC has to respond accordingly to the forcing, and this behavior is not exclusive to this basin. From a climatological perspective, it is simply
