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From | To | Subject | Date/Time | |||
COD Weather Processor | wx-storm | MESO: Mesoscale Discussion 1621 |
July 31, 2019 4:39 PM * |
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This is a multi-part message in MIME format... ------------=_1564591174-118394-2783 Content-Type: text/plain ACUS11 KWNS 311639 SWOMCD SPC MCD 311639 MEZ000-MAZ000-NHZ000-RIZ000-CTZ000-NYZ000-VTZ000-NJZ000-311745- Mesoscale Discussion 1621 NWS Storm Prediction Center Norman OK 1139 AM CDT Wed Jul 31 2019 Areas affected...Portions of the northern NJ...southern NY and much of New Enlgand Concerning...Severe potential...Watch possible Valid 311639Z - 311745Z Probability of Watch Issuance...60 percent SUMMARY...Thunderstorms are expected to increase in coverage over the next couple of hours and shift northeast across the Northeast U.S. These storms will pose a threat from strong, locally damaging winds, and a watch may be needed in the next hour or so. DISCUSSION...Strong heating ahead of a surface cold front was apparent in 16z observations from the mid-Atlantic into New England where temperatures in the mid 80s to low 90s were already being reported. Southwesterly low level flow is maintaining a very moist boundary layer, with surface dewpoints in the upper 60s to low 70s. The net result is a corridor of 1000 J/kg MLCAPE across the region. An MCV was noted in radar loops, approaching Albany NY as of 1620z. Thunderstorms were beginning to intensify on the southern flank of this feature across Ulster and Orange counties in NY, and Sussex county in NJ. Given the aforementioned downstream environment, continued intensification of these storms is expected. While effective shear remains modest (around 25 kt) some localized enhancement aided by the MCV is possible, and organized line segments capable of mainly strong, locally damaging wind gusts is possible as storms track east/northeast through the afternoon. Additional CU development was noted in visible satellite imagery across portions of CT into RI and MA where the strongest heating has occurred. A surface trough also was apparent in late surface analysis stretching from the Chesapeake Bay vicinity northeast into central ME. Convective initiation could eventually occur from the CU field, which appears to be co-located with the surface trough. Modest deep layer flow and midlevel lapse rates will temper more intense cells. However, high PW values and sufficient instability, combined with steepening low level lapse rates will support multiple bands of storms capable of strong, locally damaging wind gusts. A watch may be needed in the next hour or so across portions of the Northeast. ..Leitman/Hart.. 07/31/2019 ...Please see www.spc.noaa.gov for graphic product... ATTN...WFO...GYX...BOX...BTV...OKX...ALY...PHI...BGM... LAT...LON 40587281 40427378 40717447 41007472 41497464 41907449 42517378 43397256 44007163 44277105 44317052 44147025 43917020 43347037 42547070 41867098 41477132 41097165 40667253 40587281 ------------=_1564591174-118394-2783 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. ------------=_1564591174-118394-2783-- --- SBBSecho 3.07-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (1:2320/105) |
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