An Alberta Clipper is a fast moving system that originates around Alberta Canada. These have also been called Saskatchewan Screamers, also based on the region in Canada where they originate.
They arrive in arctic patterns and often move through very fast, with only a few hours of snowfall.
The track plays a big role for us east of the mountains.
If the center of Low Pressure (L) passes directly over Baltimore or to the north, much of the snow will sublimate and erode away. Any stickage would be west of Frederick and north of I-70 or the PA line.
If Low Pressure passes south of Baltimore, these events can bring a ‘typical’ 1 to 3 inches of snow to metro areas. The higher mountains can get in on more.
A squall line is also a fast moving snow event. These also behave much like the ‘clippers’ with location of the Low Pressure. But these can also be along an arctic front or caused by Vort Mazes, peak spin in the jet stream.
Like an intense line of thunderstorms, they may last a few minutes, but less than 1/2 hour.
A squall can produce near blizzard conditions for brief period. That means snowfall rates of 1″/Hr with winds gusting over 35 mph.
Miller A Storms are the winter events that often come from The Gulf of Mexico. These can take on new form as a coastal Nor’Easter.
The track is important as these can bring in warmer air from the Atlantic, resulting in that dreaded mix or rain on Delmarva and by the Chesapeake Bay.
Along I-95 and within about 10-20 miles can be the dividing line of snow and rain. This is explained in the Maryland Snow page.
These are one of the two Big Snow types of storms. Not all, but some can be the ones that produce double digit snowfall totals, if the conditions are right.
These can produce 10+” inches in the colder inland suburbs of central Maryland/southern PA, 1/2 that amount or less in the cities, and even less or all rain near Annapolis, southern Maryland, and the Eastern Shore.
The Miller B Storm complex can be the most complicated.
These events start with a Low Pressure in the Mid-West to Ohio Valley. Then they transfer energy to a new Low forming along the Mid Atlantic coast.
During this transition, one of two results are common:
Stay in the ‘zone’ and a long duration snow or ice event can last a few days.
Get Dry Slotted. This is when dry air from the original Low expands when moving over the mountains. That can cut off precipitation and BUST a forecast if it does not fill back in.
Often this all depends on the Strength of the original Low and the location of the new coastal Low.
These can be among the heaviest snow producers if conditions are just right. If you stay ‘in the zone’ snow can last for 2 days or longer.
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