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 |
June 29, 2024 8:04 AM * |
|||
ACUS01 KWNS 291251 SWODY1 SPC AC 291249 Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 0749 AM CDT Sat Jun 29 2024 Valid 291300Z - 301200Z ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS OVER PARTS OF THE NORTHEAST...AND OVER THE RATON MESA AND NEARBY SOUTH-CENTRAL HIGH PLAINS... ...SUMMARY... Damaging thunderstorm gusts and a few tornadoes are possible today over parts of the Lower Great Lakes to upper Ohio Valley, while severe gusts also may be focused this afternoon and evening over the Raton Mesa and nearby south-central High Plains. ...Synopsis... Broadly, the upper-air pattern will be characterized by a synoptic trough moving ashore from the Pacific and over the West Coast States, the downstream ridge moving slowly out of the northern/ central Rockies onto the adjoining High Plains, and troughing over the Great Lakes and vicinity. Meanwhile, strong subtropical ridging will prevail across the Southeast, southern Plains, and NM. A northern-stream shortwave trough -- evident in moisture-channel imagery over northeastern MN -- will eject east-northeastward today and weaken, while effectively replaced by an upstream perturbation now over portions of ND/MB. The resulting shortwave trough should proceed eastward across the Upper Great Lakes to Lake Huron and adjoining parts of ON by 12Z tomorrow. To its south and southeast, a belt of strong, cyclonically curved flow will cover the mid/upper Ohio Valley and Northeast, with minor embedded perturbations (some convectively generated upstream from prior/overnight activity). At the surface, the 11Z analysis showed a low over central Lake Superior, with cold front across central Upper MI, southern WI, southern IA, central KS, and north-central NM. By 00Z, the cold front should move to northern IN, central IL, southern MO, northern OK, the northern TX Panhandle, and northeastern/central NM. By 12Z, the front should extend from western parts of NY/PA across KY, the MO Bootheel area, and northern AR, becoming quasistationary over central/western OK, the central TX Panhandle, and east-central NM. A prefrontal surface trough should shift eastward from the St. Lawrence Valley/Lower Great Lakes across the northern Appalachians and northern Mid-Atlantic States through the period. ...Northeast/Ohio Valley/Great Lakes... Scattered thunderstorms are expected to form episodically from midday through afternoon -- predominantly ahead of the surface cold front. Frontal convection over parts of Lower MI also is possible this afternoon, with isolated severe hail/gusts. The main severe threat, however should be over parts of the Lower Great Lakes/upper Ohio Valley into nearly Appalachians. With weak capping, activity may form on a variety of foci, near the main surface trough, outflow boundaries from morning clouds/precip, and over areas of differential heating and orographic lift. Activity should organize into one or more lines with embedded supercells and bowing/LEWP segments possible. The main threat will be damaging to severe gusts in and near the 15%/"slight" area, though any supercells or embedded QLCS vortices also will pose a tornado threat. Despite weak mid/upper-level lapse rates over most of this region, warm-sector moisture will be characterized by mid 60s to lower 70s F surface dewpoints. This will combine with pockets of sustained surface heating to yield MLCAPE in the 1000-2000 J/kg range. Veering and strengthening of winds with height in low levels should yield enlarged hodographs below 3 km, with effective SRH in the 150-250 J/kg range overlapping areas of favorable heating in some parts of the upper Ohio Valley area into central PA. Little speed shear is apparent from the top of the boundary layer into the mid/upper levels, however, limiting deep shear, and storm structure may become messy rather quickly. Overall, convection should weaken as it approaches the Atlantic Coast this evening, and the foregoing inflow layer becomes more stable. ...South-central Rockies/High Plains... Isolated to scattered thunderstorms are forecast to develop this afternoon over higher terrain from the southern Front Range area across the Sangre de Cristos and Raton Mesa. This will occur as strong heating of higher terrain preferentially erodes MLCINH, in the presence of post-frontal upslope flow in low levels, and related moisture advection to at least partially offset moisture loss due to mixing. The easterly component also should aid storm-relative boundary-layer flow and deep shear for activity propagating eastward off the elevated terrain, with a mix of multicells and transient supercells possible. Despite modest low/middle-level wind speeds, forecast soundings reasonably depict enough veering with height to yield 35-45-kt effective-shear magnitudes, amidst 500-1500 J/kg MLCAPE and steep boundary-layer lapse rates. Some of the resulting convection may coalesce into a complex of thunderstorms with a cold pool, in turn driving eastward-directed forward propagation near the post-frontal moist axis and across parts of southeastern CO, northeastern NM, the adjacent Panhandles, and or southwestern KS, with a relatively focused threat of severe gusts. ...Ozarks/south-central Plains... Ongoing, isolated to widely scattered convection over parts of KS/MO should weaken/dissipate through the remainder of the morning, but may leave behind enough cloud material and (especially in MO) outflow to augment frontal baroclinicity for afternoon convective initiation. Widely scattered to scattered thunderstorms should develop on and near the front this afternoon from northern OK and extreme southern KS to the Ozarks, in a regime of MLCINH substantially removed by modest low-level convergence and strong diurnal/prefrontal heating. Deep mixing south of the front should reduce surface dewpoints and buoyancy in the warm sector, but adequate moisture (with 60s to low 70s F surface dewpoints) should linger in a narrow post-frontal corridor supporting 2000-3000 J/kg MLCAPE. The net result should be high-based, multicell thunderstorms in mostly weak deep shear, with pulse severe in the form of gusts and hail. A conditional risk exists for locally significant (65+ kt) gusts, given the favorably deep subcloud mixed layer with large DCAPE. However, mesoscale foci for denser coverage of such a threat still appear too nebulous for a 15% unconditional gust outlook within the broader marginal area. ..Edwards/Kerr.. 06/29/2024 $$ --- 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: 0.0165 seconds If you experience any problems with this website or need help, contact the webmaster. VADV-PHP Copyright © 2002-2024 Steve Winn, Aspect Technologies. All Rights Reserved. Virtual Advanced Copyright © 1995-1997 Roland De Graaf. |