Go to the Globe and Mail homepage

Jump to main navigationJump to main content

AdChoices
Heavy machinery clears snow from a street following an autumn storm in Buffalo, New York, November 20, 2014. (AARON LYNETT/REUTERS)
Heavy machinery clears snow from a street following an autumn storm in Buffalo, New York, November 20, 2014. (AARON LYNETT/REUTERS)

What caused Buffalo’s massive snow and why Toronto got lucky Add to ...

Torontonians have long been the butt of jokes about calling in the army every time a few snow flurries whip by. But the city can take comfort in knowing that it should be spared the kind of snowmageddon that befell Buffalo.

The massive storm that buried Buffalo and parts of New York State under piles of powder stems from a meteorological phenomenon called lake-effect snow, created when cold wind blows over a warmer water surface – in this case, Lake Erie.

interactive-image



While also sitting near a great body of water, Toronto is rarely struck by lake-effect snow because of its position relative to Lake Ontario.

“The founding fathers of Toronto, whether they realized it or not, did actually pick a location where we don’t get a lot of snowfall. As a matter of fact, of any major city in Ontario, Toronto gets the smallest amount of snow in an average winter,” said Geoff Coulson, an Environment Canada meteorologist.

“You’re very lucky. Very, very lucky,” said U.S. weather specialist Brett Anderson, a senior forecaster for Accuweather.com. “We’re having a second round of lake-effect [over Buffalo]. It started last night and it continues today.”

Three reasons Buffalo was hit so hard

1. Direction: The cold wind was coming in a direction that was parallel to the long axis of Lake Erie, maximizing the “fetch”, or the time and distance the cold air travels over the body of water. The direction of the low-level wind is the most significant factor in determining who’s going to get hit by these bands of snow,” Mr. Coulson said. For Buffalo, late autumn and early winter brings the most frequent lake-effect snows before Lake Erie, the shallower of the Great Lakes, ices over and reduces the exposed water surface.

2. Duration: Furthermore, Mr. Anderson said the cold wind also blew steadily for at least 30 hours. Usually the wind fluctuates within six to 12 hours.

3. Difference in temperature: The temperature difference between the air and the water was also very wide, triggering a more vigorous precipitation. Mr. Anderson said the water surface temperature was about 6C while readings in the air above went as low as –13C. The big temperature gap made for a more unstable atmosphere, triggering thundersnow, Mr. Anderson said, a phenomena corroborated by the eyewitness reports of thunder and lightning.

Could it happen in Toronto?

Unlikely – and if it did, not as severely as what happened to Buffalo.

Other parts of Ontario are more vulnerable to lake-effect snow, Mr. Coulson said. For example, southwest winds blowing over Lake Ontario regularly dump lake-effect snow on Cobourg and the Prince Edward County area, triggering multi-vehicle pile-ups on Highway 401.

The Bruce peninsula and areas east of Georgian Bay are currently facing warnings for snow squalls and lake-effect snows because they are downwind from Lake Huron.

Lake-effect snow is typically carried by band-like streamer clouds and falls in narrow bands of heavy snow. Toronto sometimes gets the tail end of lake-effect snow from Georgian Bay but those are rare and brief occurrences, Mr. Anderson said.

An east wind could also bring lake-effect snow to Toronto and Mississauga but those winds are not common, Mr. Coulson said.

Report Typo/Error

Follow on Twitter: @TuThanhHa

Next story

loading

In the know

The Globe Recommends

loading

Most popular videos »

Highlights

More from The Globe and Mail

Most popular