Author Topic: Lake Effect and Snow Squalls Explained....  (Read 3024 times)

Offline avoorpool

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Lake Effect and Snow Squalls Explained....
« on: March 21, 2013, 12:46:57 PM »
Toronto / Pickering - Canada

Surrounded by the Great Lakes of North America (NZ will fit a few times in this massive water basin  :)) has its pros and cons.......

Knowing the water supply is good for approx. 21% of the total Earth Fresh Water amount (it's expected that in the (far) future the price of Fresh Water will reach the same as Oil today  :)) weather wise it offers many surprises...!!!

Take a look at the attached Radar picture (courtesy Intellicast) taken today, first day of Spring - March 20 2013..

It's called "Lake Effect".
So how does this work???

Since this winter temperatures haven't been constantly sub-sub-sub zero, the water of the Great Lakes is NOT frozen all over, and still 'relatively' "warm" compared to outside temperatures.....
Our majority of Wind direction is N - NW, so Mr (or Mrs) Wind says: " Hey, let's pick up some "warm" water from Lake Superior, Lake Huron and Georgian Bay, and take it in our path towards South-Western Ontario, and then dump it in the form of Snow.... :o
Those bands are called "Snow Squalls", a typical weather pattern in winter, but very tricky for motorists.
They often cover only a few kilometers (see picture), so  one time you're driving in FULL Sunshine, the next moment visibility is absolutely "zero" and you're in a blast of SNOW..!!

Today was the same: Nice Sunshine at times in the afternoon and the next moment you look outside in the midst of a "Snow storm", however, it disappears as quickly as it comes.....

So, that's the "Lake Effect" in Winter for Toronto - Ontario.

Summer time has a different 'surprise', mainly in the form of extreme humidity and humidex temperatures (reaching + 45 C...)
Now I wish we were there already..  :) :)

Cheers,

Arthur 




« Last Edit: January 17, 2017, 11:04:08 PM by JennyLeez »




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