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1883 Rochester tornado

Windstorm in Minnesota, United States

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Through Tornado, Surface weather observation and Thunderstorm

Meteorological synopsis

On the morning of August 21, a mid-latitude, deepening low-pressure center moved east-northeastward toward Minnesota, crossing the state during the afternoon and evening. The following morning, the cyclone had already deepened to at most 29.42 inHg (996 mb), suggesting a robust system on the preceding day. At the time, surface weather data from the Upper Mississippi Valley were sparse, but nearby observations in the afternoon indicated high temperatures in the middle 80s to low 90s °F. Eyewitnesses reported very humid conditions, indicating ample moisture for thunderstorms to develop. As author Joseph Leonard mentioned in the History of Olmsted County, Minnesota,

At Rochester the day had been hot with a strong southeast wind, the air was smoky and oppressive, the heavens were overcast with clouds of a dull leaden line, and there were, apparently, three strata, all moving in different directions.

Although meteorology in 1883 was primitive compared with modern science, Leonard's observations and other weather reports reveal quite a bit about the atmospheric conditions in Southeastern Minnesota on August 21. High temperatures, sufficient humidity, strong surface winds, and vertical wind shear appear to have all been present—all of which are key factors in the development of tornadoes.

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