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From | To | Subject | Date/Time | |||
Mike Powell | All | DAY1SVR: Day 1 Convective |
August 25, 2024 8:57 AM * |
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ACUS01 KWNS 251257 SWODY1 SPC AC 251256 Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 0756 AM CDT Sun Aug 25 2024 Valid 251300Z - 261200Z ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS OVER PARTS OF THE FOUR CORNERS TO SOUTHWESTERN WYOMING...AND OVER PORTIONS OF WESTERN MINNESOTA AND THE EASTERN DAKOTAS... ...SUMMARY... Severe gusts and hail are most probable today over parts of the Four Corners to southwestern Wyoming, and this evening over portions of western Minnesota and the eastern Dakotas. ...Synopsis... A seasonally well-amplified mid/upper-level pattern will persist over the CONUS, but with some important changes due to the progression of embedded synoptic- to subsynoptic-scale features. An intermittently closed cyclone now over north-central NV will eject slowly northeastward to southeastern ID through the period, while devolving to an open-wave trough. By 12Z tomorrow, the full trough should extend from the MT Rockies southward through the remnant low's vorticity max, then southwestward to southern NV. Meanwhile, a broad anticyclone -- initially centered over northern OK/southern KS -- will move northeastward, with the 500-mb high over central MO by 12Z, and ridging north-northeastward across Lake Superior. The northward component of this shift should occur partly in response to a well-defined low/trough in the subtropical easterlies, now evident over the north-central to southwestern Gulf. This feature should move ashore on the lower/middle TX Coast around the end of the period. Northeast of the high, a strong shortwave trough now over northwestern QC will dig south-southeastward through tonight, reaching the St. Lawrence Valley and approaching northern NY by 12Z. At the surface, 11Z analysis showed a persistent, very slowly frontolytic, quasistationary boundary from just offshore of the Carolinas to the north-central Gulf Coast, becoming a diffuse warm front over astern parts of TX/OK. Rich low-level moisture has returned northward near this boundary in OK/AR and farther north across parts of the central/northern Plains. A low was drawn north of MIB, with cold front southwestward across the northwestern corner area of SD, into north-central WY. By 00Z, the front should reach from near the MN/ND/MB border confluence across the eastern Dakotas, parts of north-central/southwestern NE and near CYS. The front should proceed overnight to a 12Z position from northeastern MN to the FSD/SUX vicinity, central NE and eastern CO. ...Northern Plains/Upper Midwest... Scattered thunderstorms are expected to develop along/ahead of the cold front -- predominantly after 00Z, though enough moistening/ heating may occur for isolated late-afternoon development. Supercells and bowing lines/clusters will be possible, offering large hail and severe gusts. Activity should occur as the front encounters what is left of a diurnally well-heated and still-unstable boundary-layer airmass, with only minimal diabatic cooling, due to the presence of rich moisture near the surface, Surface dewpoints already are commonly in the 70s F in a swath of the warm sector with 11Z axis from north-central ND south-southeastward across eastern portions of SD/NE/KS and the Arklatex region. Forecast soundings indicate the moist layer should deepen through the day beneath strong capping, and steep midlevel lapse rates. With a deep troposphere still present over this area, atop the favorably unstable boundary layer, MLCAPE in the 3000-4000 J/kg range will be possible. This will be collocated with slowly strengthening flow aloft, such that 30-45-kt effective-shear magnitudes will be possible from late afternoon through the evening. ...Central/southern Rockies and vicinity, south-central Plains... Scattered showers and thunderstorms, with at least isolated strong-severe gust potential, should become common by this afternoon in a vast, roughly triangular area in and near the outlook, from western NM and eastern AZ to parts of southeastern MT and southern KS. Within that area, the greatest potential for severe should be on the western fringes, with supercells and bowing clusters possible in a corridor spanning portions of the Four Corners area to southwestern WY. In that region, the greatest diurnal destabilization will overlap the most favorable deep-layer lapse rates, and strengthening vertical shear ahead of the progressive western trough. Mid/upper-level moisture-channel imagery, available GPS PW data, and surface analysis show a persistent plume of deep-layer monsoonal moisture, maintaining some continuity from the ITCZ well south of mainland MX, across parts of west-central MX and Chihuahua, to NM, CO, WY and western NE. Enough low-level moisture (PW above 1 inch in some areas) to support organized convective potential extends farther westward over the Four Corners area, especially into northeastern AZ, eastern UT and western CO. Forecast soundings in that corridor show favorable deep shear for supercells, with effective-shear magnitudes in the 40-55-kt range, and elongated, rather straight low/middle-level hodographs favoring a large-hail threat, in addition to the broader severe-gust potential. Farther east, much of the higher terrain across the "marginal" area will reach convective temperature relatively early in the diurnal-heating cycle, with little CINH, resulting in abundant development, slowing the pace of additional destabilization. Still, isolated strong/briefly severe gusts may occur, especially where north-northeastward moving clusters of convection encounter pockets of well-mixed boundary layer suitable for intense downdrafts. Farther east onto the High Plains, more-favorable heating/mixing will occur, but with weak shear nearer to the mid/upper high. ..Edwards/Bentley.. 08/25/2024 $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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