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nonintensifying TCs have no such link ( Merrill 1988a ). Recent research has further demonstrated that outflow tends to develop in regions where upper-tropospheric inertial stability is low, and stronger outflow tends to be associated with intensifying TCs ( Rappin et al. 2011 ; Barrett et al. 2016 ; Komaromi and Doyle 2017 ). Synoptic-scale forcing has been found to further reduce upper-tropospheric inertial stability, which favors intensification ( Rappin et al. 2011 ). Additionally, eddy flux convergence
nonintensifying TCs have no such link ( Merrill 1988a ). Recent research has further demonstrated that outflow tends to develop in regions where upper-tropospheric inertial stability is low, and stronger outflow tends to be associated with intensifying TCs ( Rappin et al. 2011 ; Barrett et al. 2016 ; Komaromi and Doyle 2017 ). Synoptic-scale forcing has been found to further reduce upper-tropospheric inertial stability, which favors intensification ( Rappin et al. 2011 ). Additionally, eddy flux convergence
