


Severe Storm Outlook Narrative (AC)
Issued by NWS
Issued by NWS
350 ACUS03 KWNS 170732 SWODY3 SPC AC 170731 Day 3 Convective Outlook NWS Storm Prediction Center Norman OK 0231 AM CDT Tue Jun 17 2025 Valid 191200Z - 201200Z ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS FROM NEW ENGLAND INTO THE MID ATLANTIC... ...SUMMARY... Strong to potentially severe thunderstorms are forecast on Thursday from parts of New England into the Mid Atlantic and Carolinas. ...Synopsis... A seasonably deep mid/upper-level trough is forecast to move across parts of southeastern Canada and adjacent portions of the northeast CONUS on Thursday. In conjunction with this trough, a surface cyclone is expected to move from southeast Ontario into southern Quebec, as a trailing cold front moves through parts of the Northeast/New England and the Mid Atlantic. To the west, an upper-level ridge will continue to build from the southern Rockies into parts of the central Great Plains, with multiple midlevel shortwave troughs expected to move from the Great Basin into the northern Rockies and High Plains along the periphery of the ridge. ...Parts of New England southward into the Mid Atlantic, Carolinas, and Southeast... Rich low-level moisture will already be in place across parts of the Carolinas and Mid Atlantic Thursday morning, with some northward moisture transport expected through the day along/ahead of the approaching front. Guidance continues to vary somewhat regarding timing of the front, and also the extent to which stronger mid/upper-level flow lags behind the front. However, in general, moderate destabilization is expected into at least southern New England by afternoon, and perhaps farther north depending on lingering cloudiness and frontal timing. Scattered thunderstorm development will be possible along/ahead of the front from the Carolinas/Mid Atlantic into New England during the afternoon. Wind fields will generally be stronger with northward extent. Depending on the extent of destabilization, supercells and organized clusters will be possible across parts of New England and perhaps the northern Mid Atlantic, which would pose some threat of all severe hazards. Farther south into the southern Mid Atlantic and Carolinas, deep-layer shear will be weaker, but favorable low-level moisture, strong buoyancy, and modest midlevel southwesterlies will support outflow-driven clusters capable of damaging winds and possibly some hail. The organized severe threat will tend to decrease with southwestward extent, due to weaker deep-layer flow. However, favorable low-level moisture and buoyancy could support a few strong to locally severe storms along the trailing cold front into parts of the Southeast during the late afternoon and evening. ...Parts of the Upper Great Lakes/Midwest... In the wake of the departing mid/upper-level shortwave trough, modest lingering low-level moisture beneath relatively cool temperatures aloft may support moderate diurnal destabilization across parts of the Upper Great Lakes and Midwest. Some guidance develops southeastward-moving convection across parts of northeast MN into northern WI during the afternoon, possibly in response to a midlevel jetlet approaching the Upper Midwest from the northwest. This scenario is uncertain, but moderate midlevel northwesterly flow and sufficient deep-layer shear would support at least an isolated severe threat if convection can be sustained during the afternoon and evening. Other strong storms may develop Thursday night within a warm-advection regime. ...Northern Plains... Increasing low-level southerly flow will aid in low-level moisture return across parts of the central/northern Plains on Thursday. Strong diurnal heating will result in MLCAPE increasing above 2000 J/kg into parts of the Dakotas and Nebraska. Wind profiles will support organized convection, and MLCINH may be mostly eroded by late afternoon, though potential for storm development into evening is highly uncertain, given the presence of rising midlevel heights and generally limited large-scale ascent. Later Thursday evening into the overnight, a nocturnal low-level jet may aid in elevated storm development, though the details of any severe threat associated with this potential late-period convection remain uncertain at this time. ..Dean.. 06/17/2025 $$