Minor edit: replaced Ned Stark with a Whitewalker
The cold promised by a northeast winter is finally here. The storm that dropped 2-4 inches of rain on Thursday night has exploded into a large midlatitude cyclone and is still slowly meandering to the NE over NE Canada. Cold air will continue flowing in behind the storm, dropping temperatures below normal.Infrared satellite imagery of the Northwestern Atlantic showing a large low pressure system over Eastern Canada with cold front associated convection (thunderstorms extending into the Caribbean |
So about that snow:
The upper levels of the atmosphere are well cold enough for snow. The problem is available moisture and lift. Both are lacking on the back side of a low pressure system, where dry continental winds push out of the NW. So how are we going to get moisture? It lies with the Great Lakes and its famous lake effect snow.
Wind and water are important to lake effect. A cooler, ice covered lake in the winter will require air to travel over it for a longer time to pick up the same amount of moisture as wind traveling over a warm lake. Wind that is perpendicular to the lake will move air over the lake for too little time to pick up enough moisture but strong flow parallel to lake length is the best setup for lake effect. That is why cities at the eastern ends of the lakes, like Buffalo and Watertown, NY are such good places for lake effect. In cold winters, when the lake finally freezes over, the lake effect tap is turned off for the rest of the season.
How lake effect works |
NAM model at 1AM Tuesday depicting two lake effect precipitation bands (mostly rain) coming off Lake Huron with some enhancement by lake Ontario. |
The next chance for snow will come as the cold air mass retreats ahead of the next storm early Thursday morning. Moisture will overrun the cold airmass. There is a good chance of some snow showers ahead of the main slug of moisture warms the atmosphere enough to change over to rain. Unfortunately, (or fortunately, I'm a snow nut) the approach of the low will direct southerly winds at us, warming us well above freezing, but not past 50 on Thursday. Slight changes in moisture transport and storm track could have visible effects on precipitation types. In my experience, (though confined to DC area snowstorms) precip tends to start a few hours earlier than predicted. However, since it is still early in the season, it's going to be hard to get substantial snow. Even then, some good snowTV would be pretty to go with the cold.
GFS model prediction for 8AM Thursday showing a bit of snow before changing over to rain |
-Alex
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