Do You Miss Buffalo?

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I was just on the phone with my dad. We talked about the weather a little. He’s in Milwaukee where it’s 29 with a wind chill of 22. My office window thermometer shows 72.

“Bet you’re glad you’re not in Buffalo,” he said.

I am.

766 Auburn Ave   Google Maps

I lived here, at 766 Auburn Avenue (Google streetview link) in the third floor apartment. It was a beautiful one bedroom with no insulation and enough water pressure to take a shower if no one in the other two apartments was! During the summer we were woken by squirrel races on the roof.

Those who live in Buffalo do so by choice. Anyone who wanted to leave left a long time ago. There is a survivor spirit among the residents.

It is a really nice, liveable city. Real estate is very reasonable. Summers are magical. Winters are hellish.

Starting in mid-November a thick veil of low clouds descends upon the city. This is the beginning of the process that spawns Lake Effect snow. It’s convection, like bubbles in a pot of boiling water. It will remain mainly cloudy with a handful of exceptions until spring.

This time of year the Great Lakes are warm and the flow through the atmosphere cold. Warm air near the lake’s surface is drawn up, condensing as it cools. Clouds form, often dropping snow.

Lake Effect season begins suddenly. The start is when the potential for big storms is greatest… as we saw this past week. Once Lake Erie freezes the process shuts down.

Lake Ontario doesn’t freeze. Sorry Syracuse.

For a real Lake Effect event, winds must be aligned through the atmosphere often parallel to a lake’s longest dimension.

These storms are VERY localized. The physics involved in Lake Effect snow is very similar to summertime thunderstorm formation. In fact, sometimes thundersnow is part of a Lake Effect storm.

Think “thunderstorm downpour” of snow… except instead of moving on, the storm continues for hours or days relentlessly.

aurora

This graph is from East Aurora, NY. Under land use it’s marked, “Urban.” People live there. That’s over 30″ of snowpack with a water equivalent of 5″.

The edges of Lake Effect storms are well pronounced. You drive out of Lake Effect snow like you drive out of a summer thunderstorm. And these boundaries stay in place as long as the wind doesn’t shift.

No one can cope with this much snow. No one is equipped, even those areas that get as much as 200″ of snow a year!

“Yes, Dad. I’m glad I’m not in Buffalo.” But I don’t regret a day of living there.

Buffalo And The World’s Weirdest Weather

The photo at the top of this entry is Buffalo, Wednesday afternoon. The Sun is shining brightly.

Wondering where the snow is?

Elmwood-Avenue

The photo at the top of this entry is Buffalo, Wednesday Tuesday afternoon. It’s my old neighborhood on Elmwood Avenue. The Sun is shining brightly.

Wondering where the snow is?

robhimself793: I’m about a mile from the snow band, I have very little snow, maybe 6″. Just a mile south and people have 3 feet.

You’re seeing one of the more interesting aspects of Lake Effect snow. It is VERY localized. There’s heavy snow just a few miles from where this image was captured.

Lake Effect snow is the product of convection. Heat and moisture are transferred upward into the clouds from the relatively warm lake. You can see that in this time lapse of Lake Erie, one of the coolest pieces of weather video I’ve ever seen.

Heavy Lake Effect snow needs cold wind roughly parallel to the lake to get going. The resulting storm forms slender ‘streamers’ which reach out from the lake. They are often just a few miles wide, with flurries at the edges and white out conditions in the middle!

Near the Great Lakes it’s possible to drive from no snow to 4″/hour conditions in just two or three miles! These bands can stay stationary for hours, or even days!

Buffalo gets a lot of snow each winter, over 90 inches! Because of Lake Effect there are heavier snowbelts south of the city. People in Buffalo scratch their heads why anyone would want to live there, as we scratch our heads over Buffalo.

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