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From | To | Subject | Date/Time | |||
Mike Powell | All | DAY1SVR: Day 1 Convective |
September 29, 2024 9:54 AM * |
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ACUS01 KWNS 291230 SWODY1 SPC AC 291228 Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 0728 AM CDT Sun Sep 29 2024 Valid 291300Z - 301200Z ...NO SEVERE THUNDERSTORM AREAS FORECAST... ...SUMMARY... Severe thunderstorms are not forecast for today. ...Synopsis/Discussion... A highly amplified, slow-moving, mid/upper-level pattern will persist over much of the CONUS, south of a progressive northern stream near and north of the Canadian border. A norther-stream trough, nearly synoptic in scale, is apparent in moisture-channel imagery from central/southwestern BC to near-coastal WA/OR. This feature should amplify and move eastward across southwestern Canada and the interior Northwest through the period, reaching east- central/south-central SK, central MT and western WY by 12Z tomorrow. Weak, basal height falls and modest midlevel moisture will contribute to the potential for isolated, high-based convection over portions of UT, some of which may extend deep enough to generate lighting and strong gusts, into a deeply mixed boundary layer. Weak moisture/buoyancy (MLCAPE generally less than 100 J/kg) precludes an unconditional severe area. As the northern-stream trough moves away from CA, a formerly cut-off low now moving ashore into south-central CA will become cut off again, and drift southward/southwestward back toward the Pacific by the end of the period. Ridging will weaken greatly over the northern Plains and Upper Midwest ahead of the northern-stream trough, but will persist at its root over the Four Corners region. To its east, a longstanding, stacked, gradually filling cyclone will drift erratically eastward over the TN/KY border area, possibly devolving into an open-wave trough by the end of the period. Associated convection to its east will encounter a relatively warm/ stable layer in mid/upper levels, limiting but not entirely suppressing potential for convection to reach into icing layers suitable for lightning. As such, isolated thunder will be possible from the central Appalachians to the Tidewater. Although warm midlevels will extend southward to most of FL, rich boundary-layer moisture/theta-e south of a quasistationary frontal zone over northern FL will support sporadic thunderstorm potential, mainly from midday through early evening. ..Edwards/Broyles.. 09/29/2024 $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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