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From | To | Subject | Date/Time | |||
Mike Powell | All | DAY1SVR: Day 1 Convective |
August 6, 2024 9:08 AM * |
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ACUS01 KWNS 061300 SWODY1 SPC AC 061258 Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 0758 AM CDT Tue Aug 06 2024 Valid 061300Z - 071200Z ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS OVER MUCH OF MONTANA INTO WESTERN SOUTH DAKOTA...AS WELL AS FROM PARTS OF LOWER MICHIGAN INTO NEW JERSEY...THE COASTAL CAROLINAS...AND ACROSS PARTS OF ARIZONA... ...SUMMARY... Severe-thunderstorm potential exists today over much of Montana into western South Dakota, as well as from parts of Lower Michigan into New Jersey, the coastal Carolinas, and across parts of Arizona. ...Synopsis... In mid/upper levels, a longstanding, large, western CONUS anticyclone -- centered initially over southern CO -- is expected to become more compressed on the northern and southwestern fringes, while the center retrogrades back across the Four Corners region. This will occur in response to shortwave developments in the northern stream and subtropical easterlies. For the latter, a well- defined trough is evident in moisture-channel imagery over portions of southern NM, far west TX, and northwestern MX, with an embedded low over west-central Chihuahua. The trough should proceed westward through the period, reaching western Sonora and southern AZ by 12Z tomorrow. North of the mid/upper high, an accelerating, nearly zonal northern stream is forecast from the interior Northwest to the northern Upper Midwest, as heights fall south of a progressive synoptic trough over western/central Canada. This will take an initially slow-moving shortwave trough over coastal WA/OR and accelerate it eastward into the northern Rockies around 00Z, then to eastern MT by the end of the period. Another, weaker perturbation now near the CA/OR/NV border junction should accelerate northeastward today as well, preceding the Northwest trough in an eastward-turning path across southern MT. This perturbation should reach the central Dakotas by 12Z. Farther downshear, a convectively enhanced shortwave trough with embedded MCV is evident over the southern Lake Michigan region. This feature should move eastward across Lower MI and southern ON to the Lower Great Lakes by 00Z, then across the northern Mid-Atlantic and most of New England by 12Z. At the surface, 11Z analysis showed a wavy, quasistationary front from a low near ORD east-southeastward across northern portions of IN/OH/PA to southeastern NY and coastal southern New England. A cold front extended from the low southwestward over northern MO, east-central KS, to an elongated low-pressure area over the southern KS/CO border vicinity. The low is expected to migrate eastward along the frontal zone and weaken today, but perhaps slower than model progs, given the presence of the MCV/shortwave trough supporting it. By 00Z, the frontal zone should extend from near the southern New England Coast across central/northern PA and northern OH, while moving south as a cold front across central IN, southern IL, the Ozarks, to central/western OK, becoming quasistationary again to a low over southeastern CO. Surface cyclogenesis is expected late tonight across eastern WY, effectively replacing the prior southeastern CO low along a lee trough. ...Great Lakes to northern Mid-Atlantic... Scattered thunderstorms -- both discrete and in clusters -- are expected near the frontal zone today from the southern Upper Great Lakes eastward. The initial activity is apparent over southern Lower MI ahead of the shortwave trough. This includes an intense, heavy-precip supercell that may maintain a tornado threat on the north end of a favorably unstable environment in the frontal zone, juxtaposed with strong low-level shear. Upscale growth into a bowing clusters also may occur, following the frontal-related instability gradient east-southeastward. See Tornado Watch 604 and related SPC mesoscale discussions for near-term coverage. This activity, or later/foregoing development near the front, will encounter favorably moist and gradually more unstable/heated inflow air today. Supercells and bowing clusters will remain a threat, with all severe hazards possible. Surface dewpoints along and south of the front -- as well as a sort distance to its north -- will remain in the upper 60s to low 70s F (locally higher) over the outlook corridor, offsetting modest mid/upper-level lapse rates to yield MLCAPE in the 1500-2000 J/kg range. Enhancements to low-level and deep shear are expected in the mass response immediately preceding the shortwave trough, combining with backed surface winds along and north of the front to contribute to 150-300 J/kg effective SRH from southern Lower MI into northernmost OH, shifting into western PA later this afternoon. One or two corridors of relatively dense/greater damaging wind potential may develop within the current 15%/"slight" area, depending on timing/intensity of convective-cluster evolution. ...Northern/central High Plains and adjacent foothills... A couple rounds of strong-severe thunderstorms are possible across the northern High Plains: 1. Convection developing by midafternoon over higher terrain of southwestern MT, moving northeastward to eastward over southern/central MT the remainder of the afternoon into evening. Activity may aggregate upscale to a mainly wind-producing MCS with sporadic severe gusts, though isolated, marginally severe hail may occur as well. This convection should form as a zone of increasing large-scale lift (preceding the leading/weaker shortwave trough mentioned above) superimposes favorable diurnal heating of higher terrain and related preferential removal of MLCINH. This convection should move into lower elevations characterized by deep, well- heated/mixed boundary layers, but with enough low-level moisture to maintain and perhaps strengthen the convection as it crosses the outlook area. Activity should encounter progressively more-stable inflow air eastward into the western Dakotas tonight, leading to weakening. 2. Development over the northern Rockies and adjacent foothills of northwestern MT from late afternoon into evening, proceeding eastward to east-southeastward across northern MT, with large hail and locally strong-severe gusts possible. Compared to farther south, expect somewhat more low-level moisture, in a pocket of favorable boundary-layer theta-e undisturbed by the slightly earlier activity to the south and southeast, as well as stronger deep shear (45-50-kt effective-shear magnitudes) in support of supercell potential. Peak MLCAPE of 500-1200 J/kg is expected, supported by lower-elevation surface dewpoints commonly in the 50s F, and residual steep low-level lapse rates from diurnal heating. Long, relatively straight hodographs will support hail potential from any sustained supercells -- either left- or right-moving (with splitting storms possible). Eastward extent of the threat into tonight is uncertain, given the potential for outflow from the higher-based, drier-rooted southern complex to advect into the path of this activity somewhere over central to northeastern MT. ...AZ... Widely scattered to scattered thunderstorms are expected to form this afternoon over the higher terrain of north-central through southeastern AZ, roughly from east of IGM southeastward past the SAD area, as well as on some of the smaller ranges to the south of the Mogollon Rim. Activity should move over deserts/valleys to the west and southwest across southern AZ, offering areas of strong-severe gusts as outflows aggregate and additional, discretely propagating development occurs atop the cold pools. As the northern MX mid/upper trough shifts westward, height falls and a somewhat tightened mid/upper gradient will shift westward over southern AZ, leading to regional enhancement of midtropospheric easterlies to influence convective motion and ultimate forward propagation. Large-scale ascent/DCVA also is expected in advance of the trough, overlying diurnally heated/deeply mixed boundary layers to ensure steep deep-layer lapse rates. Sufficient low-level moisture (9-13 g/kg mean mixing ratios) will remain through the vertical-mixing process to support 1000-1500 J/kg preconvective MLCAPE, as well as pulses of newer development when forced ascent occurs above outflow. These processes should drive outflow, with channels of locally severe wind, across south-central/southwestern AZ and potentially into the lower Colorado River Valley and into portions of southeastern CA, before activity dissipates tonight. ...Coastal Carolinas... The threat for a few tornadoes will continue through today, and perhaps into the evening, as T.S. Debby moves very slowly eastward to northeastward, per NHC forecasts. With Debby potentially moving slightly offshore, the cyclone should maintain substantial southeasterly inflow from a large, favorably high-theta-e boundary layer over the Gulf Stream. Within its northeastern quadrant, and seaward of a large area of stabilizing rain a short distance inland, the development of sporadic middle/outer-band supercells will remain possible offshore, with tornado potential for roughly a couple counties inland until cells encounter more prohibitively low-buoyancy inflow air. Roughly 150-300 J/kg effective SRH and favorably enlarged hodographs will support this threat. See SPC Tornado Watch 603 and related mesoscale discussions for the latest near-term guidance on tornado potential. Refer to NHC advisories for the latest track/intensity guidance for Debby, as well as tropical watches/warnings. ..Edwards.. 08/06/2024 $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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