A powerful storm system will continue to bring heavy mountain snow, rain, and high winds to the Pacific Northwest and northern California through midweek. Heavy rain and flash flooding potential exists across the central Gulf Coast over the next few days, including the Florida Panhandle. A Slight Risk (level 2 of 4) of excessive rainfall is in effect Tuesday. Read More >
State College, PA
Weather Forecast Office
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. |
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SPC Mesoscale Convective Discussions |
MCD #1569 Courtesy: NWS SPC |
MCD #1571 Courtesy: NWS SPC |
MCD #1573 Courtesy: NWS SPC |
Radar
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
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.
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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US Dept of Commerce
National Oceanic and Atmospheric Administration
National Weather Service
State College, PA
328 Innovation Blvd, Suite 330
State College, PA 16803
(814)954-6440
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