


Severe Storm Outlook Narrative (AC)
Issued by NWS
Issued by NWS
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390 ACUS01 KWNS 170051 SWODY1 SPC AC 170050 Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 0750 PM CDT Sat Aug 16 2025 Valid 170100Z - 171200Z ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS ACROSS PARTS OF NORTHERN AND CENTRAL SOUTH DAKOTA AND SOUTHERN NORTH DAKOTA... ...SUMMARY... A small organized cluster of thunderstorms with potential to produce a swath of strong to severe wind gusts still appears possible across parts of the central Dakotas later this evening into the overnight hours. More sporadic strong thunderstorms with potential to produce severe wind and hail are possible in a corridor across the Midwest into Great Lakes vicinity. ...01Z Update... In the wake of a weakening convective perturbation shifting east-southeastward through the Great Lakes region, modest mid-level height rises across eastern portions of the northern Great Plains will gradually overspread the Upper Midwest and adjacent Great Lakes region overnight. In the presence of weak and/or weakening deep-layer shear, and weak mid/upper support for convective development, the probabilities for the evolution of a sustained organized severe storm cluster appear to be lowering. However, weak low-level warm advection to the immediate cool side of convective outflow, and a quasi-stationary frontal zone extending roughly from west-northwest of the Dubuque IA vicinity into the middle Missouri Valley, is forecast to contribute to a corridor of increasing thunderstorm development overnight. Although mid-level profiles appear relatively warm, a plume of dry lower/mid-tropospheric air with steep lapse rates may contribute to a risk for localized strong wind gusts and some hail in sporadic stronger storms. Upstream, across the middle Missouri Valley, as a weak mid-level short wave trough slowly shifts eastward into the western Dakotas, models continue to suggest that associated scattered thunderstorm development may gradually consolidate into an organizing cluster, perhaps aided by lift associated with warm advection on the nose of a strengthening southerly low-level jet. As this occurs, although deep-layer mean wind fields will remain generally weak, modest shear and thermodynamic profiles with steep lower/mid-tropospheric lapse rates and sizable CAPE may contribute to potential for the development of strong to severe wind gusts overnight. ..Kerr.. 08/17/2025 $$