Tropical moisture continues to flow across portions of the Great Basin, desert Southwest and California. Isolated instances of flash flooding remains possible. Meanwhile, a storm and associated frontal boundary will focus showers and thunderstorms for the center of the nation. For New England, dry and breezy conditions could enhance favorable fire weather conditions. Read More >
Overview
In the wake of a cold front resulting from the remnants of Hurricane Beryl, a convective severe weather threat existed for North-Central, Central, and South-Central PA. Straight-line wind gusts were the primary impact, though radar-indicated tornadoes/circulations were present over North-Central PA. A mid-level cap (milder air aloft), despite all other severe weather parameters being in place, kept the storms shorter and storms weaker. |
![]() Courtesy: NWS SPC |
SPC Mesoscale Convective Discussions |
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MCD #1569 Courtesy: NWS SPC |
MCD #1571 Courtesy: NWS SPC |
MCD #1573 Courtesy: NWS SPC |
Radar
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The first line of convection initiated around 11:00 AM EDT (15:00 UTC) roughly 100 miles East of the cold front. | Peak tornadic activity took place around 2:30 PM EDT (18:30 UTC), though most of this occurred in upstate NY. | Near Landisburg, KCCX imagery showed a MARC (Mid-Altitude Reflectivity Convergence) signature indicative of strong downbursts. |
Storm Reports
Environment
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Figure 1: The strong cold front associated with post-tropical storm Beryl is seen in the 18z surface analysis. The line of convection is indicated as a squall line in this analysis. Courtesy NWS WPC |
Figure 2: The cold front moved Eastward. Courtesy NWS WPC |
Near-storm environment summary.
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Figure 4: 7PM EDT Downdraft CAPE Courtesy NWS SPC |
Figure 5: 2:00 PM EDT Storm Relative Helicity Courtesy NWS SPC |
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