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1905 Snyder tornado

1905 F5 tornado in Oklahoma

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Meteorological synopsis

The tornado was caused by a strong low pressure system that developed across the Rocky Mountains, near Denver, Colorado. Another storm was also located across Wyoming on May 9. Tornadoes formed on that day across several Plains states including Missouri, Oklahoma, and Kansas. The Colorado storm system then moved toward the Central and Southern Plains on the next day and affected areas slightly to the east of the area affected on May 9. A new trough of low pressure developed in the vicinity of the southern storm. It later moved across the Oklahoma and Texas Panhandles.

As happened on numerous other occasions, such storms produced a large moist and warm flow from the Gulf of Mexico as well as much instability in the atmosphere. Being in May, storm systems produced large contrasts of temperatures, which added more ingredients for the development of powerful thunderstorms with possible damaging tornadoes. Such was the case on May 10, 1905.

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