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Hazardous Heat Across the Western U.S.; Heavy Rain and Flooding in the Southwest and Western Gulf Coast

Dangerous heat will persist over portions of interior California, the Great Basin, and the northern Rockies through Thursday. Heat will gradually spread into the northern Plains today. Across the western Gulf Coast, heavy to excessive rainfall will persist through mid-week. Additionally, the Southwest Monsoon will continue to bring a flash flooding threat to the Four Corners Region this week. Read More >

Overview 

On the evening of December 8th, strong (~1036 mb) high pressure was centered from the Great Lakes to the Mid-Atlantic. At the same time, an area of low pressure was strengthening across the southeast while an upper level shortwave was moving from the southern Plains to the mid-south. The area of low pressure became centered over the Florida Panhandle as a cold air damming regime set up across interior parts of Virginia and the Carolinas, with winds (largely) out of the NNE. A large area of precipitation was impacting the Carolinas and was approaching southern VA by sunrise on the 9th. Precipitation quickly overspread most of the CWA by Sunday morning, with snow in most areas except for coastal SE VA/NE NC, where NE winds ushered in milder, maritime air. As the shortwave approached the Mid-Atlantic region, an area of 700-500 mb frontogenesis set up from W to E just south of VA/NC border around sunrise on 12/9. While light to moderate snow was reported in most areas, bands of heavy snow (rates of 1-2"/hour) set up in/near the 700-500 mb FGen axis over far southwestern portions of the Wakefield CWA. This FGen axis would serve as the focal point for the heaviest snow bands throughout the day. It is important to note that the dendritic growth zone resided in the upper part of the 700-500 mb layer (see KRIC soundings in the Environment section for more detail).

The milder, maritime airmass slowly moved from SSE to NNW throughout the day as the surface low tracked NNE just off the southeast coast. At the same time, the 700-500 FGen axis slowly moved northward. As a result, snow started changing to sleet then rain over SE VA/northern NC Sunday afternoon. The snow became heavy over central and western portions of the CWA (including the Richmond metro area) during the afternoon where temperatures remained slightly below freezing from the sufrace-850mb. Moderate to heavy snow continued throughout the afternoon from the Richmond metro to the Virginia Piedmont. This is where a widespread 9 to 14 inches of snow was reported. Snow finally changed to sleet over the central/southern Richmond metro area between 5-8 PM before the entire area of rain/sleet/snow started to weaken as drier air filtered in from the north. The snowfall resulted in numerous flight cancellations at area airports. Interstates became snow covered and numerous accidents were reported. The 11.5 inches of snow at Richmond International Airport (measured by a COOP Observer in nearby Varina) ranks as the 2nd largest December snowstorm on record (behind only the 17.2 inches that fell on Dec. 22-23, 1908).

See the Observations, Radar, and Environment sections for more specific details about the exact location of the meteorological features mentioned above. 

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