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From | To | Subject | Date/Time | |||
Mike Powell | All | DAY1SVR: Day 1 Convective |
September 6, 2024 8:10 AM * |
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ACUS01 KWNS 061247 SWODY1 SPC AC 061246 Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 0746 AM CDT Fri Sep 06 2024 Valid 061300Z - 071200Z ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS ACROSS MUCH OF OHIO TO THE OHIO VALLEY... ...SUMMARY... Strong to locally severe storms are possible this afternoon from Lake Erie across much of Ohio to the Ohio Valley. ...Synopsis... A highly amplified mid/upper-level pattern will persist across the CONUS, but with some weakening of the western mean ridge and intensification of troughing over the Great Lakes/Ohio Valley regions. The latter will occur in relation to a synoptic-scale trough with several accompanying vorticity maxima and broad cyclonic flow -- apparent in moisture-channel imagery over much of northern ON and the Lake Superior vicinity. Phasing of accompanying shortwaves/ vorticity lobes will contribute to both amplification and wavelength shortening through the period. A closed 500-mb low should develop around 00Z near the eastern end of Upper MI, with trough near an MKG-ORD-MVN line. By 12Z, a fully developed cyclone should cover much of ON from the southern end of James Bay to Lake Erie, with 500-mb trough extending southwestward near a CVG-BNA line. Associated cyclonic flow at that time will cover most of the CONUS over and east of the mid/upper Mississippi Valley. At the surface, a cold front related to the ON trough was drawn at 11Z near a DTW-FDY-IND-ICT line. This front should proceed eastward/southeastward across the Ohio Valley, Lower Great Lakes and into the central/northern Appalachians through the period, ahead of the mid/upper trough. By 00Z, the front should extend from Lake Ontario across western parts of NY/PA to southeastern OH, northern middle to western TN, and AR, becoming diffuse amidst northeast flow on both sides over OK. Northeasterlies over the southern Plains south of the cold front will be largely in isallobaric response to a deepening surface frontal-wave low over the northwestern Gulf, initially drawn about 100 nm south of GLS, and forecast to drift erratically eastward through tonight. Strong/organized convection related to the Gulf cyclone is expected to remain over water through the period. ...OH, Ohio Valley... Damaging to isolated, marginally severe gusts, as well as marginal hail, will be possible with thunderstorms moving eastward across the outlook area today. A broken line of convection -- including widely scattered non-severe thunderstorms -- is apparent this morning from northwestern OH to western MO approximately along the low-level cold front. This activity, or succeeding/newer development after a short time gap later this morning -- should become better organized between Lake Erie and the Ohio Valley around midday as the foregoing boundary layer (and prospective inflow) destabilizes. This will occur in response to a combination of warm advection and diurnal heating/ mixing, whose mixing-related moisture-reduction effects will be counterbalanced to some extent by moist advection. Activity should move into a narrow corridor of 50s to mid 60s F surface dewpoints, combining with diurnal heating to support patchy, highly variable MLCAPE in the 500-1500 J/kg range. Substantial westerly component to prefrontal near-surface flow will limit both convergence and vertical shear, though weak MLCINH will permit frontal development/maintenance of thunderstorms, regardless. Around 30-35 kt effective-shear magnitudes will support mainly multicells, though some intermittent/transient supercell character will be possible for longer-lived, discrete cells. Activity should weaken this evening as it moves eastward out of the most favorable moisture, and into a nocturnally cooling/stabilizing boundary layer. ..Edwards/Kerr.. 09/06/2024 $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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