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The 1991 Halloween blizzard was a powerful storm that caused a period of heavy snowfall and ice accumulation, which affected parts of the Upper Midwest of the United States, from October 31 to November 4, 1991.
A prolonged and widespread tornado outbreak affected a large portion of the United States in late-May 2013 and early-June 2013. The outbreak was the result of a slow-moving but powerful storm system that produced several strong tornadoes across the Great Plains states, especially in Kansas and Oklahoma.
As a file created by an employee of the NWS (formerly USWB) in the course of their official duties, whether hosted on weather.gov; on an NWS sub-branch website ...
Great Cyclone at St. Louis, May 27, 1896 (NOAA) Photos; The Great Cyclone at St. Louis and East St. Louis, May 27, 1896 (St. Louis Public Library) Look Back: Massive tornado, landmark buildings help shape fast-growing 1890s and On this date: Great Cyclone of 1896 killed 255 and Great Cyclone of 1896 (St. Louis Post-Dispatch) The 1896 Tornado!
The 1974 Xenia tornado was a violent F5 tornado that destroyed a large portion of Xenia and Wilberforce, Ohio, United States on the afternoon of April 3, 1974. It was the deadliest individual tornado of the 1974 Super Outbreak, the 24-hour period between April 3 and April 4, 1974, during which 148 tornadoes touched down in 13 different U.S. states.
The tornado outbreak of June 5–6, 2010, was a tornado outbreak that affected the Midwestern United States and Great Lakes region, starting the weekend of June 5, 2010, and extending into the morning of June 6, 2010.
The Advanced Weather Interactive Processing System (AWIPS) is a technologically advanced processing, display, and telecommunications system that is the cornerstone of the United States National Weather Service's (NWS) operations.
On June 16, 2010, an upper-level area of low pressure and associated trough moved southeastward across the Rocky Mountains into the Great Plains.Along the base of the trough, the presence of a strong mid-level jet stream provided significant instability; however, warm-air aloft was expected to limit the extent of convective development.