|
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 | DAY2SVR: Nws Storm Predic |
September 12, 2025 9:25 AM * |
||
ACUS02 KWNS 120601 SWODY2 SPC AC 120600 Day 2 Convective Outlook NWS Storm Prediction Center Norman OK 0100 AM CDT Fri Sep 12 2025 Valid 131200Z - 141200Z ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS FOR PARTS OF THE SOUTHERN AND CENTRAL HIGH PLAINS AND THE NORTHERN PLAINS... ...SUMMARY... Strong to severe storms are possible over parts of the southern and central High Plains and northern Plains Saturday. ...Synopsis... The western upper trough will continue its slow progress eastward on Saturday. The trough is expected to eject into central Plains by early Sunday morning. A few embedded shortwave troughs will pivot into the northern Plains and stronger mid-level winds will extend into the southern Rockies. At the surface, a low in the northern Plains will become more diffuse during the period. ...Southern/Central High Plains... On the southern edge of the broad western trough, stronger mid-level flow will be perpendicular to the southern Rockies into part of the Front Range. Low-level moisture will advect into the regions given surface southeasterly winds. Moisture will be greatest in New Mexico with mid/upper 50s F dewpoints. Farther north, flow will become much more meridional and moisture will be more limited. Within the southern Rockies, cloud cover associated with the trough will generally keep low-level lapse rates weak. However, modestly steep mid-level lapse rates with the cooler air aloft and 35-40 kts of effective shear will promote some risk for a few supercell structures by the afternoon. Isolated large hail will be the main risk. While a similar hail threat will be present for much of the Front Range, this area is also more likely to receive greater surface heating. Steeper low-level lapse rates will support a threat for isolated severe gusts with the strongest storms. ...Northern Plains... Scattered thunderstorms will likely be ongoing at the start of the period. By this time, steeper mid-level lapse rates will likely have diminished for much of the western Dakotas into eastern Montana and Wyoming. This activity will be driven by a northward moving shortwave trough and low-level warm advection. Despite cloud cover complicating the low-level thermodynamic environment and the surface low gradually weakening with time, there may still be zone of greater potential in the eastern Dakotas where steeper mid-level lapse rates will be. Greater shear/forcing will overlap greater buoyancy during the afternoon in this area as well. The strongest storms, if they develop, will likely be near and east of the Missouri River. Small to isolated marginally severe hail appears to be the primary hazard. ...Upper Midwest... A weak shortwave trough is expected to move through southern Wisconsin into the southern Lake Michigan vicinity. This will promote a zone of warm advection that will allow potentially scattered storms to develop. While shear will be modestly enhanced with the shortwave, greater buoyancy and lapse rates will be displaced to the west. A stronger storm or two could occur, but limited confidence in greater severe storm coverage precludes probabilities. ..Wendt.. 09/12/2025 $$ --- SBBSecho 3.28-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. |
