A particularly strong and prolonged PRE (rainfall totals >200 mm) occurred on 25 September 2005 in the upper Midwest as TC Rita made its way from the Texas/Louisiana coast northward into the central U.S. A widespread region of heavy rain (radar echoes ~4050 dBZ) stretching from western South Dakota through southern Minnesota and into western Wisconsin developed and persisted for ~36 h as a substantial, poleward surge of deep, tropical moisture (precipitable water values ~40 mm) impinged upon a quasi-stationary, southwestnortheast-oriented baroclinic zone. A distinguishing characteristic of this PRE event was its quasi-stationary nature. It is hypothesized that downstream tropospheric ridging associated with TC Rita served to enhance the poleward moisture transport and acted to create a midtropospheric flow pattern that promoted slow system propagation.
The purpose of this presentation is twofold: First, it will assess the synoptic-scale environment in which the 25 September 2005 PRE occurred in the upper Midwest with particular emphasis on the central role of TC Rita in the persistent supply of tropical moisture to this region. Second, it will document how the dynamic and thermodynamic structure of the environment in the vicinity of the PRE evolved to favor exceptionally heavy rain over the upper Midwest.