The number of RI events in this offshore area has shown an increasing trend since 1980 due to more favorable thermodynamic environments (higher relative humidity and maximum PI), reduced vertical wind shear, global ocean warming, the influence of the Pacific Decadal Oscillation, anthropogenic forcing, and landward migration of TC activity ( 15 ).
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Synergistic impact of marine heat waves and rapid intensification exacerbates tropical cyclone destructive power worldwide.
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