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From | To | Subject | Date/Time | |||
COD Weather Processor | wx-storm | DAY1SVR: Day 1 Convective Outlook |
August 3, 2019 12:55 PM * |
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This is a multi-part message in MIME format... ------------=_1564836930-118394-4523 Content-Type: text/plain ACUS01 KWNS 031255 SWODY1 SPC AC 031254 Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 0754 AM CDT Sat Aug 03 2019 Valid 031300Z - 041200Z ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS OVER PARTS OF THE NORTHERN PLAINS... ...SUMMARY... Isolated strong to severe thunderstorms are possible this afternoon over the northern High Plains. ...Synopsis... The upper-air pattern will continue to feature a stout anticyclone centered over the southern Rockies, with ridging northward across the central Rockies and northern High Plains. A strong shortwave trough -- apparent in moisture-channel imagery over the Canadian Rockies -- should move eastward across much of SK by the end of the period. A lesser perturbation -- initially over central/eastern MT -- will move eastward through the mean ridge to central ND by 00Z. At the surface, 11Z analysis showed a quasistationary frontal zone from south-central New England across central PA, becoming diffuse over much of the Ohio Valley, then better-defined again from the Ozarks to the central Dakotas. A moist axis was drawn just to the west of the boundary across the central/northern Plains. This boundary should remain near its present locations except where overtaken tonight by a cold front moving southward from QC across NY and New England. ...Northern Plains... Isolated to widely scattered thunderstorms are expected to develop this afternoon near the ND/MT line and south-southwestward over northeastern WY, in a zone of favorably strong surface heating, and near a surface trough located west of the moist axis. Activity should move eastward to southeastward into stronger moisture for a few hours, with isolated large hail or strong-severe gusts possible. The minor perturbation and associated cloud cover should pass over the area before peak afternoon destabilization. This will render two somewhat counterbalancing effects: 1. Relatively unimpeded, strong surface diabatic heating, producing steep low-level lapse rates in an environment of at least marginally favorable low-level moisture, with MLCINH essentially eliminated in some spots. 2. Weak large-scale subsidence, or at best, near-neutral vertical- motion fields in midlevels by late afternoon. Height falls related to the peripheral influence of the Canadian trough should wait unto tonight, and will be subtle. These factors call into question the coverage of convection, through buoyancy should be favorable, with surface dew points 60s F contributing to a narrow corridor of MLCAPE in the 1000-2000 J/kg range (locally/briefly higher). Effective-shear magnitudes 30-35 kt are forecast with nearly straight hodographs, indicating a blend of multicellular and splitting/brief supercell modes possible. Convection should diminish markedly after dark as appreciable large-scale forcing for ascent, preceding the major shortwave trough, remains north of the international border. ...Southern OK to central TX... Isolated hail briefly near severe levels cannot be ruled out in the next couple hours from a core or two within a lengthy plume of convection training southward across southern KS and eastern/ southern OK into north TX, until the supportive warm-advection regime weakens diurnally. The potential appears too isolated/ conditional for an outlook area. Isolated to widely scattered thunderstorms may develop this afternoon across southern OK and north TX, a few of which may produce strong gusts. The most favorable instability is expected south and west of the early cloud cover over parts of central TX, as strong surface heating weakens MLCINH and deepens/mixes the boundary layer. However, low-level forcing and convective coverage in that regime appears questionable. Meanwhile, extensive cloud cover is evident in satellite imagery and should linger over much of the area of greatest deep-layer support. As such, an unconditional outlook is not being re-introduced at this time due to lingering concerns over convective coverage/organization, as well as the lack of more- substantial vertical shear. However, the well-mixed boundary layer will offer some cause for concern if enough storm coverage can accumulate to organize cold pools. Mesoscale trends will be monitored for a better-organized, stronger wind threat than currently evident. ...Eastern PA to southern New England... Widely scattered thunderstorms are possible this afternoon in a west-southwest/east-northeast corridor along and south of the front. This area will reside within the northern rim of a corridor of favorable low-level moisture and diurnal heating south of the boundary. Surface dew points commonly in the mid/upper 60s F in lower elevations, and MLCAPE near 1500 J/kg may support a few strong multicells with downdrafts approaching severe levels. However, weak low/middle-level winds will substantially limit vertical shear. While minor damage cannot be ruled out in the most intense cores, the potential for severe/50+ kt wind appears too small and conditional for a categorical area at this time. ..Edwards/Broyles.. 08/03/2019 $$ ------------=_1564836930-118394-4523 Content-Type: text/plain; charset="US-ASCII" Content-Disposition: inline Content-Transfer-Encoding: 7BIT = = = To unsubscribe from WX-STORM and you already have a login, go to https://lists.illinois.edu and use the "Unsubscribe" link. Otherwise email Chris Novy at cnovy@cox.net and ask to be removed from WX-STORM. ------------=_1564836930-118394-4523-- --- SBBSecho 3.07-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (1:2320/105) |
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