National Weather Service United States Department of Commerce

Powerful Storm in the Western U.S.; Heavy Rain and Flooding Threat Across the Central Gulf Coast

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 >

Overview

The storms produced lots of large hail and some wind damage. Most of the severe weather happened along and south of Route 22 between 3 PM and 8 PM. The storms fried up along a pre-frontal surface trough that had developed ahead of a cold front which was moving southward through PA during the afternoon and evening. Many of the storms exhibited low-level rotation, and had strong storm-top divergance - indicating strong updrafts and mesocyclones. Storm tops on this day over PA reached up to 50 kft at times, with most up to 40 kft. Steep mid-level lapse rates (the rate of cooling as you move up in elevation) and a freezing level around 11 kft provided a good set up for large hail. The worst storm of the bunch was a rotating supercell over Cumberland County. The storm moved through Carlisle about 5 PM, producing very large hail and some wind damge. The low-level rotation was so strong that a tornado warning was issued for central Cumberland County. See the reflectivity and storm-relative motion images from the KCCX 88D below. Inferring the storm structure from the reflectivity panels below, there is a (bounded) weak-echo region (BWER) over and just to the south of Bloserville. This is coincident with the best low to mid-level rotation on the SRM pics. These signatures pair up to indicate a strong, rotating updraft holding lots of water aloft. The area in the storm where the large hail is falling is most likely between Bloserville and Carlisle at 2053 UTC (453 PM EDT). There is a weak hook echo on the SW edge of the storm, which is most likely the base of the mesocyclone (the rotating updraft). A very noticable three-body scatter spike (hail flare) is visible extending SE out of the storm (away from the radar). This signature is another strong indication of a storm with lots of hail being held aloft. There is so much power reflected back to the radar in those radials that the radar has trouble specifying a distance and azimuth of the strong returns due to the hail stones themselves bouncing the radar energy around inside the storm core before returning it to the radar site. Hail of up to 2 inches was reported from this storm as it continued to move SE through northern York County and the western edge of Lancaster County.

ImageImage

nws logo Media use of NWS Web News Stories is encouraged!
Please acknowledge the NWS as the source of any news information accessed from this site.
nws logo