How Do Winter Storms Form, and Where?
Winter Storms - One name for many forms of extreme weather.They may differ in name and form, but they are all disruptive.
The topic is a large and complex one. Some types of winter storm occurregularly each season, sometimes more than once, and have beengiven their own names - Alberta Clipper, Nor'easter, Panhandle Hook. Others, just as severe, are not so romantically named.
But rather than describe each type of storm, let's look for some common ground. When you want to find out more about the events which affect you most often, wander on over to
The Weather Doctor's
A Few Basic Facts and Principles
I'm sorry to do this to you, but most winter storms have a number of features in common, so let's set the scene.
But first, let's clear up the term "storm". For our purposes, a storm is any disturbed state of the atmosphere affecting the earth's surface, accompanied by unpleasant or destructive weather. In scale a storm ranges from an individual thunderstorm to hurricanes or even larger extra-tropical
depressions. Low pressure, usually as an enclosed low,
is associated with many of them.
Winter storms fit in towards the larger end of the scale, particularly as far as the area affected is concerned.
Not the best of definitions I guess, but the overall complexity of storms prevents a simple definition
So let's set the stage for storm formation. Here are some basic
weather and climate fundamentals.
Storm formation is complex enough even within this scenario (and this is by no means the full story), and the factors listed above also apply reasonably well to eastern Europe. But now let's add in the effect of the Rocky Mountain chain.
Many of the surface disturbances develop over the northern Pacific and move east to the North American mainland. But when they hit the Rockies, they are forced up and around, losing much of their moisture content and energy as rain and snow is dumped. Many retain enough of their character to reform on the eastern side of the mountains, and start all over again as a significant storm.
(Europe has no significant chains of north - south mountains to
interrupt the movement of weather systems.)
So during winter we have a group of lows forming in the northern
Pacific, reforming over or past the Rockies, and moving on to
affect the northern and northeastern USA and Canada.
A second group of winter storms forms in the Gulf of Mexico and western Atlantic.These storms track up the eastern side of the USA, varying from inland of the Appalachians to 200-300 miles (300-500km) out to sea.
Of course these two groups can find many ways to interact, and
that is often when things get really interesting.
Winter Storms with a Western Origin
Eastern Pacific storms have two sources. Many of them originate
in the relatively warm maritime polar airmass, particularly
in the Gulf of Alaska. High mountains around the Gulf restrict
these Gulf of Alaska Lows, causing them to move off to the south to ultimately cross the coast anywhere between Canada and California. Perhaps helped along by the jetstream, they are forced to rise over the Rockies, dumping their contained
moisture as they cool, as either rain or snow.
The second source is more a means of moving weather than a
storm in itself. It is associated with the subtropical jetstream
and because it arrives from the direction of Hawaii, is called the Pineapple Express. This fast moving stream of warm, very
moist air can meet the west coast anywhere from southern
Canada to California, and is capable causing very high
rainfall and snow as it rises over the Rockies.
Mix the Pineapple Express with a Gulf of Alaska Low and it's
time to dust off the record books.
In crossing the Rockies these storms have lost most of their
moisture, but still have the capacity to reform. Although this
can happen anywhere, there are two main centres for regeneration
- Alberta and Colorado.
Gulf of Alaska Lows form rapidly and follow each other quickly,
and so do Alberta Clippers. The name comes from the fastest of
the nineteenth century sailing ships. They form around the Alberta plains and head off along the polar front, generally passing into Montana or North Dakota before heading east towards the Great Lakes and New England and the Maritime
Provinces of Canada.
Because they have lost most of their moisture and have little
access to more, they are rarely responsible for heavy rain or snow - 2 to 4 inches on the northern side of their path is about the norm. They are usually followed by very cold northerly winds, and their rapid generation can result in some long spells of rather miserable weather.
Alberta Clippers can result in heavy Lake Effect snows on the
lee sides of the Great Lakes, and although they are otherwise
not usually responsible for much new snow, their strong winds
can cause blizzards as previously fallen snow is picked up
and moved around.
Colorado Lows and Panhandle Hooks
Pacific storms often reform around Colorado. When the jetstream is in its normal position and travelling east around the Canadian border, these and other winter storms forming in the
southern Rockies will normally track east, pick up some moisture from the Gulf of Mexico, and cause a little rain and
But when the jetstream loops south, the Colorado Lows and
the related Texas Panhandle Hooks head off to the north or
northeast and have the potential to cause serious problems.
They follow the polar front and jetstream north, picking
up plenty of moisture from the gulf maritime air to the east.
Circulation around the low pressure center brings strong
northerlies, including the Blue Norther of southern states,
with potentially large snowfalls to the west of the storm's
path. Characteristic paths for these large winter storms include the Ohio valley, and strong winds and large snowfalls for the
Chicago - Great Lakes area are possible.
These storms are also likely to move on to New England and the Canadian Maritime Provinces.
East Coast Storms
A large group of winter storms affecting the east, and particularly
northeast Atlantic coast of the USA and Canada are known as
Nor'easters, after the direction of the winds bringing the worst of the rain, strong winds, and snow.
In keeping with the rule that nothing is simple, Nor'easters
can form in several ways, have a wide range of paths ranging
from inland to well offshore, and have the potential to
virtually explode into devastating events ("The Perfect
One group of storms forms in the Gulf of Mexico or nearby
western Atlantic. Depending on source and location of
mid continent highs or jetstreams, these storms can move
along the western margin of the Appalachians, along the
coastal plain, or anywhere within a few hundred miles off
Typical of winter storms, snow is likely to fall to the
left of the storm's track, with rain more likely to the right. Storms moving north over the ocean will usually
produce snow in coastal areas (to their left) as they
are continually picking up moisture from the relatively
warm sea surface, often including the Gulf Stream. Other
storms form off Cape Hatteras and move in the same way.
Some Nor'easters, particularly those intensifying off New
England or eastern Canada, may be the remnants of Alberta
Clippers, Colorado Lows or Panhandle Hooks. Normally these
systems will move off rapidly to the east to be seen no more, but other scenarios are possible.
If, for example, a Colorado Low runs into a Nor'easter
moving north along the coast, or even an extra-tropical
low moving in from further out in the Atlantic, an
extremely powerful storm can grow very rapidly. Winter storms
such as these are responsible for huge dumps of snow
from New York northward, hurricane force winds, and
huge seas accompanied by storm surges. These weather
bombs or bomb cyclones can form in other ways, but
their characteristic is rapid development of a very
Winter storms are a great field for observation and study
by the owner of a home weather station.
For a start, no matter where you live in North America, you
would expect to see several reasonable winter storms each year between the beginning of fall and the end of spring, whereas
a hurricane or severe thunderstorm may be rare or nonexistent
in many regions.
Secondly, most winter storms take a while to build up, pass through and decline, giving plenty of time to assemble records.
Thirdly, with the sort of weather likely in most winter storms
you probably will be staying home with enough time on your hands
to indulge in a bit of weather study.
And finally, depending on where you are in relation to the storm's
path, the sequence of weather and trends in observed data may be
quite different even though the type of storm is the same.
The topic of Winter Storms covers a wide variety of weather
patterns and types of threatening, if not
While many websites cover warmer weather events like hurricanes
and tornadoes, winter weather doesn't attract quite the same
The Weather Doctor
provides a large number of informative and entertaining articles on many aspects of
winter weather. For an overall, concise view work your
way through the weather section of
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Last update 05/28/2011