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 | DAY1SVR: Day 1 Convective |
December 27, 2024 9:16 AM * |
||
ACUS01 KWNS 271244 SWODY1 SPC AC 271243 Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 0643 AM CST Fri Dec 27 2024 Valid 271300Z - 281200Z ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS ACROSS PARTS OF THE CENTRAL GULF COAST STATES... ...SUMMARY... A few strong to locally severe thunderstorms could occur today across parts of the central Gulf Coast States. ...Synopsis... In mid/upper levels, a broad area of cyclonic flow will persist around mean troughing, from the Great Basin and Rockies across the Great Plains to the Mississippi Valley. The leading shortwave trough -- in a series of them to influence convective potential through early next week -- is apparent in moisture-channel imagery over the MO Bootheel southward over portions of the Mid-South region. This feature will weaken considerably as it ejects northeastward to OH by 00Z, in response to an upstream trough initially over the southern/central Plains to Black Hills and western Dakotas. That higher-amplitude perturbation will reach the eastern Dakotas, lower Missouri Valley and Ozarks by 00Z, then eject northeastward to the Upper Great Lakes by the end of the period. A third shortwave trough -- currently moving inland from the Pacific Northwest Coast -- should dig southeastward rapidly across the Great Basin, reaching the southern High Plains and Permian Basin regions by 12Z tomorrow. At the surface, 11Z analysis showed a low over the western Ozarks between SGF-HRO, with occluded front arching across the Mid-South to west-central MS, warm front over south-central MS to near MOB then southeastward across the FL Keys. A slow-moving cold to quasistationary front was drawn from west-central MS across the southwestern LA coastline and TX shelf waters to a weak low over Padre Island. The low should move north-northeastward to northern WI by 12Z tomorrow, with frontolysis occurring to its south near the Mississippi Valley. Cyclogenesis will occur overnight over northwest TX in advance of the third mid/upper-level shortwave trough. ...Portions of central Gulf Coast region... Multiple rounds of convection are expected through this evening, with the best-organized cells offering locally strong-severe gusts and a marginal tornado risk. This includes a couple bands of ongoing convection -- along a dominant western convergence zone just ahead of the cold front, from eastern to southwestern MS and coastal south-central LA, and another near I-59 in southern MS. The 12Z LIX sounding sampled the coastal airmass between these well, with MLCAPE around 1400 J kg, effective SRH around 270 J/kg, modest winds between 250-500 mb, and effective-shear magnitude near 30 kt. With the leading trough ejecting away from the area and weakening fast, and the next remaining stronger but passing abeam of the outlook area to the north, net height changes through most of the period should be near neutral, with some rises possible in the near term (indicating the ongoing activity is unlikely to get substantially better organized than at present). However, a progressive lobe of midlevel vorticity -- extending southeastward from the second trough -- will foster large-scale DCVA/lift late this afternoon into evening over portions of MS and northern/western AL before the lobe ejects away and dissipates. This will be well-timed with peak afternoon warming, to steepen low-middle-level lapse rates and weaken MLCINH, contributing to potential regeneration/strengthening of the western convective/ convergence band. That process, with 60s F warm-sector surface dewpoints between the cold and warm fronts, should contribute to 1000-2500 J/kg MLCAPE. Deep shear and low-level hodographs should favor at least isolated supercells, with 35-45-kt effective-shear magnitudes and 200-300 J/kg effective SRH (maximized near the warm front). However, by mid/late afternoon, deep ascent and shear will have peaked over most of the area. With increasing displacement between the stronger flow/forcing aloft related to the second trough, and the favorable boundary-layer airmass, already marginal severe potential should diminish overnight. ..Edwards/Grams.. 12/27/2024 $$ --- 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: 0.0198 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. |