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Ice storms Winter storms: Formed: January 11, 2007: Dissipated: January 24, 2007: Lowest pressure: 961 millibars (28.4 inHg) [1] Maximum snowfall or ice accretion: 4 inches (10 cm) of ice (Oklahoma, Missouri), 32 inches (81 cm) of snow (Gaspe Peninsula) Fatalities: 85+ total: Damage: $380 million: Areas affected: Eastern, Central United States ...
The Mid-December 2007 North American winter storms were a series of two winter storms that affected much of central and eastern North America, from December 8 to December 18, 2007. The systems affected areas from Oklahoma to Newfoundland and Labrador with freezing rain , thunderstorms , sleet , snow, damaging winds, and blizzard-like conditions ...
The February 2007 North American blizzard was a massive winter storm that affected most of the eastern half of North America, starting on February 12, 2007, and peaking on Valentine's Day, February 14.
It was the snowiest day in decades at William P. Hobby Airport in Houston, where 3 inches of snow fell, according to NWS data.The last time that much snow fell in the area was in 1949. FOX Weather ...
The National Weather Service (NWS) issued winter storm warnings and winter weather advisories for much of Oklahoma on Sunday, December 13, warning drivers of dangerous conditions due to heavy ...
The AOL.com video experience serves up the best video content from AOL and around the web, curating informative and entertaining snackable videos.
Extratropical cyclone pumping subtropical moisture into the Southwestern United States December 1, 2007. A low-pressure system developed across the southwestern United States on November 30 and brought significant rainfall for portions of the Desert Southwest as well as portions of southern California from Los Angeles to the Mexico border, where destructive fires took place in October 2007 ...
At the Austrian alpine village of Galtür, snow on the mountains surrounding the village build up. Due to the changing temperature during the month, a strong but brittle layer of ice forms under the snow. On the day of the disaster, the ice layer collapses and the building ice bank slips down the slope and forms a powder avalanche.