AT2k Design BBS Message Area
Casually read the BBS message area using an easy to use interface. Messages are categorized exactly like they are on the BBS. You may post new messages or reply to existing messages! You are not logged in. Login here for full access privileges. |
Previous Message | Next Message | Back to General Weather-related Discussi... <-- <--- | Return to Home Page |
|
||||||
From | To | Subject | Date/Time | |||
![]() |
Mike Powell | All | DAY2 3/5 RISK AREAS POSTE |
May 15, 2025 9:18 AM * |
||
ACUS02 KWNS 150530 SWODY2 SPC AC 150529 Day 2 Convective Outlook NWS Storm Prediction Center Norman OK 1229 AM CDT Thu May 15 2025 Valid 161200Z - 171200Z ...THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS FRIDAY AFTERNOON INTO FRIDAY NIGHT ACROSS PARTS OF NORTHEASTERN ARKANSAS...EAST CENTRAL AND SOUTHEASTERN MISSOURI...SOUTHERN ILLINOIS...SOUTHERN INDIANA...SOUTHWESTERN OHIO...MUCH OF WESTERN AND CENTRAL KY...WESTERN AND MIDDLE TENNESSEE... ...SUMMARY... Severe thunderstorms appear likely to develop across parts of the middle Mississippi through lower and middle Ohio Valleys Friday afternoon into Friday night. During the late afternoon into evening, this may include a few intense supercells posing a risk for large hail and tornadoes. During the evening into the overnight hours, this probably will include an upscale growing and organizing cluster posing a risk for strong, damaging winds and perhaps a continuing risk for tornadoes. ...Discussion... Downstream of a prominent mid-level high over the southern mid- to subtropical latitudes of the eastern Pacific, split flow will persist across much of North America through this period. Within this regime an initially deep and occluded surface cyclone, centered over northern Minnesota at the outset of the period, is forecast to weaken Friday through Friday night, as it migrates into the Upper Great Lakes region in response to a short wave perturbation pivoting around the southern periphery of the mid-level circulation center. It appears that this perturbation will come in phase with another short wave perturbation forecast to accelerate east-northeast of the central Great Plains through much of the Ohio Valley by early Saturday. Another vigorous short wave trough digging around the northeastern periphery of the Pacific ridge may reach the northern California coast by the end of the period, preceded by at least one more modest perturbation migrating northeastward across the northern Baja vicinity. In lower levels, associated with the occluding cyclone, a weak/weakening Pacific cold front/dry line appears likely to stall across the lower Great Lakes through Ohio River vicinity, and across the Ark-La-Tex into Rio Grande River by 12Z Friday. This may be trailed by another weak front across the Upper Midwest through the central Great Plains and Texas South Plains, which is forecast to be overtaken by the primary cold front surging southeastward from the upper Mississippi Valley/northern Great Plains. By late Friday night, this cold front may reach the lower Ohio Valley and central Great Plains. Preceding the consolidating fronts, low-level moisture return and moderate to strong destabilization is forecast across the middle Mississippi and lower Ohio Valleys on strengthening south to southwesterly flow. The potential northern extent of the moisture return remains unclear, based on model output, and this could be impacted by outflow associated with possible early period convective development across the lower Ohio Valley into portions of the Allegheny and Cumberland Plateaus. Depending on how these uncertainties play out, it might not be out of the question that a more substantive outbreak of severe thunderstorms could evolve than currently depicted. It is possible areal coverage and probabilities could be increased further in later outlooks for this period. ...Lower Great Lakes into northern Mid Atlantic... Uncertainty lingers concerning the potential for severe weather. However, the intersection of the initial weak surface cold front/dryline and warm front could still be providing a focus for strong to severe thunderstorm development at the outset of the period across the lower Great Lakes/upper Ohio Valley vicinity. Aided by continuing inflow from better potential instability across the Ohio Valley, in the presence of moderate to strong vertical shear, it is possible that this could continue into the day Friday, perhaps evolving into an organizing cluster which should tend to propagate southeastward and perhaps pose potential for strong to severe surface gusts. ...Middle Mississippi into Ohio Valley... There remains at least some signal that a modest short wave perturbation, within the belt of westerlies emanating from the subtropical eastern Pacific, may be contributing to vigorous convective development at the outset of the period, or shortly thereafter, across parts of the lower Ohio Valley. If this occurs, it might not be out of the question that the boundary-layer downstream, into the western slopes of the Appalachians, might destabilize in time to support an upscale growing cluster with potential to produce to produce severe wind and hail. The impact of this possible early period convection might be the primary contributor to at least some continuing model disparity concerning upstream boundary-layer moistening and destabilization (particularly the northern extent) across the middle Mississippi into lower Ohio Valleys. However, it still appears most probable that destabilization, as far north as the I-44 corridor of central/eastern Missouri, will support the initiation of storms by early afternoon, in response to forcing for ascent associated with the mid-level perturbation emerging from the central Great Plains. This is generally forecast to shift east-northeastward into the lower Ohio Valley through late Friday afternoon, in an environment that may support at least a window of opportunity for sustained/long-lived supercells with potential to produce large to giant hail and a couple of strong tornadoes. Into Friday evening and overnight, there remains a considerable signal in model output that large-scale forcing for ascent will support a notable upscale growing and organizing cluster, in the presence of seasonably strong (and increasingly convectively augmented) westerly deep-layer mean flow. This may support widespread severe surface gusts, occasionally in excess of 65 kt, across a swath from southern Indiana/western Kentucky and northern Tennessee toward the Allegheny and Cumberland Plateaus. ..Kerr.. 05/15/2025 $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
||||||
|
Previous Message | Next Message | Back to General Weather-related Discussi... <-- <--- | Return to Home Page |
![]() Execution Time: 0.0137 seconds If you experience any problems with this website or need help, contact the webmaster. VADV-PHP Copyright © 2002-2025 Steve Winn, Aspect Technologies. All Rights Reserved. Virtual Advanced Copyright © 1995-1997 Roland De Graaf. |