Today, were are focused on the Upper Mississippi Valley for severe convective development. A potent, negatively-tilted shortwave trough is moving quickly across the north-central U.S. Strong deep-layer shear associated with the trough should combine with moderate (to strong) instability and deep moisture to produce severe convection, including supercells. It is uncertain, however, whether sufficient heating can occur in the wake of a late-morning mesoscale convective system across eastern Minnesota and western Wisconsin. If destabilization can occur in the vicinity of the residual outflow boundary, tornadoes will be possible.
A secondary area of interest is in south-central Nebraska, where the surface front curves to the southwest. In this area, the moisture is both deep and quality; the instability , strong to extreme; and the winds at the surface should back, augmenting — to some extent — the marginal wind shear. That said, severe hail and winds should be the primary threats.
We will start operations in the Minneapolis (MN), Sioux Falls (SD), and Hastings (NE) county warning areas, with an eye toward the Duluth (MN) CWA — should destabilization occur.
-G. Garfield, Week 5 Coordinator