Abstract

Abstract The synoptic-scale evolution during the formation phase of a midtropospheric cutoff cyclonic circulation over the eastern United States is diagnosed within the potential vorticity framework using the GALE (Genesis of Atlantic Lows Experiment) case of 18–19 January 1986. The study examines 1) the precursor flow evolution prior to cutoff cyclone formation; 2) the wind, mass, and potential vorticity evolution during the 2-day period encompassing cutoff formation; and 3) the relative contribution of upper-versus lower-tropospheric forcing on the quasigeostrophic height tendency field prior to and during cutoff formation. The primary large-scale features prior to cutoff cyclone formation are an amplifying ridge over the western United States and eastern North Pacific and a diffluent trough over the central United States. The primary smaller-scale feature prior to cutoff formation is a short-wave trough-jet streak system that propagates through the longer-wave-amplifying ridge, and then intensifies upo...

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