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1985 United States-Canadian tornado outbreak

1985 United States-Canada tornado outbreak
1985-05-31 tornado outbreak map.PNG
Tracks of all tornadoes that touched down during the outbreak
Type Tornado outbreak
Duration May 31, 1985
Tornadoes confirmed 44 confirmed
Max rating1 F5 tornado
Duration of tornado outbreak2 ~8 hours
Damage $980 million (2005 USD)
Casualties 90 fatalities, hundreds of injuries
Areas affected New York, Ohio, Pennsylvania, Ontario

1Most severe tornado damage; see Fujita scale

2Time from first tornado to last tornado

1Most severe tornado damage; see Fujita scale

The 1985 United States – Canada tornado outbreak, referred to as the Barrie tornado outbreak in Canada, was a major tornado outbreak that occurred in Ohio, Pennsylvania, New York, and Ontario, on May 31, 1985. Forty-four tornadoes were counted including 14 in Ontario, Canada. It is the largest and most intense tornado outbreak ever to hit this region, and the worst tornado outbreak in Pennsylvania history in terms of deaths and destruction.

The upper air pattern was conducive for a major severe weather event in the Great Lakes that Friday, May 31. An unseasonably deep low pressure system at 984 hPa crossed out of the Midwestern U.S. through the day, and then into the Upper Peninsula of Michigan. Very warm air surged in ahead of this system. Temperatures reached the upper twenties in Celsius (approximately 80-85 Fahrenheit) across much of southern Ontario, in addition to high dew point levels. An unstable atmosphere (surface based lifted indices around minus 6) was the byproduct of this. Directional wind shear was also present in the warm sector of the storm, in addition to high helicity values and a vorticity maximum approaching the lower lakes.

The situation was worsened by the presence of copious amounts of moisture, which would allow any storms that could form to become severe rather quickly. Also, this was supportive of the HP (high-precipitation) counterpart of the supercell thunderstorm (Verkaik, 1997). All of this added up to the distinct possibility of severe rotating storms that were messy, hard to see, and extremely dangerous. What was needed now was a trigger, and that came in the form of a trailing cold front behind the low. Severe thunderstorms and isolated tornadoes had already raked parts of the Midwest U.S. (particularly in Iowa and Wisconsin) the day before on May 30, associated with this same cold front (Grazulis, 1990).

The day started off on an active note with the warm front moving northwards. A possible tornado was reported near Leamington, accompanied by golfball size hail from widespread severe thunderstorm activity in southwestern Ontario. Following the warm frontal passage, skies cleared rapidly and temperatures quickly began to rise. The cold front began crossing Lake Huron towards the noon hour, and with it several thunderstorms developed shortly after 1:30pm EDT, with the northernmost cell soon becoming most dominant. Environment Canada issued a severe thunderstorm warning at 2:25pm for Bruce County (complementing the special weather statement issued early that morning). At around 2:50pm, an F2 tornado touched down briefly in the Lion's Head area (north of Wiarton) before moving out over Georgian Bay and dissipating.


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