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D. M. Rodgers, M. J. Magnano, and J. H. Arns

inhibited Gulf moisture flux into thecentral states, thus limiting the number of MCCsduring this normally active time of year.3. Case examples The following selection of four case examples illustratcs that large mesoscalc convective systems maybe spawned within a variety of synoptic flow regimes.Each example is discussed in regard to the positionof the MCC relative to midtroposphcric features asrevealed in 500 mb analyses. Of course, a number ofconditions must co-exist to support MCC development

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