The PV slots were narrow, but amenable to analysis using model output and observational data. Although the main track of large-scale PV flow was located near the US-Canadian border, a small, weaker branch of the PV current formed well south of this track in northwest flow directed across Colorado toward Arkansas. An old frontal boundary at the surface lifted prefrontal air containing high values of convective potential energy initializing convection in the path of the PV slot aloft. Thunderstorms that formed in the path of the PV slot quickly grew into organized convective systems resulting in a succession of heavy rain events.
We will present several diagnostic computations (using observations as well as high resolution model output) in an attempt to describe the development of these systems. Because they developed within the profiler array, there is an opportunity to use hourly wind data to describe a vorticity budget in good temporal detail and, if other thermodynamic analyses are adequate, a potential vorticity budget in lesser detail.
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