Winter storm

A winter storm is a type of precipitation in which the dominant varieties of precipitation are forms that only occur at cold temperatures, such as snow or sleet, or a rainstorm where ground temperatures are cold enough to allow ice to form (i.e. freezing rain). In temperate continental climates, these storms are not restricted to the winter season, but may occur in the late autumn and early spring. Also, there are very rare occasions that they form in summer, though it would have to be an abnormally cold summer, such as the summer of 1816 in the Northeast United States of America. In many locations in the Northern Hemisphere, the most powerful winter storms usually occur in March and, in regions where temperatures are cold enough, April.

Snowstorms

Snowstorms are storms where large amounts of snow fall. Snow is less dense than liquid water, by a factor of approximately 10 at temperatures slightly below freezing, and even more at much colder temperatures. Therefore, an amount of water that would produce 2 cm (0.8 in.) of rain could produce as much as 20 cm (8 in.) of snow. Five centimeters of snow (2 in.) is enough to create serious disruptions to traffic and school transport (because of the difficulty to drive and maneuver the school buses on slick roads). This is particularly true in places where snowfall is uncommon but heavy accumulating snowfalls can happen (e.g., Atlanta, Seattle, London, Memphis, Canberra). In places where snowfall is common, such as Buffalo, New York, and Minneapolis, such small snowfalls are rarely disruptive, though snowfalls in excess of 15 cm (6 in.) usually are.

A massive snowstorm with heavy winds is known as a blizzard. A large number of heavy snowstorms, some of which were blizzards, occurred in the United States during the early and mid-1990s, and the 1993 "Superstorm" was manifest as a blizzard in most of the affected area.

Large snowstorms can be quite dangerous: a 15 cm (6 in.) snowstorm will make some unplowed roads impassable, and it is possible for automobiles to get stuck in the snow. Snowstorms exceeding 30 cm (12 in.) will cave roofs of some homes and cause the loss of power. Standing dead trees can also be brought down by the weight of the snow. Even a few inches of dry snow can form drifts of many feet high under windy conditions.

Secondary dangers

Snowstorms are usually considered less dangerous than ice storms. However, there are secondary dangers of the ambient snow that may result from a snowstorm. Mountain snowstorms can produce cornices and avalanches. An additional danger, following a snowy winter, is spring flooding if the snow melts suddenly due to a dramatic rise in air temperature. You can also die from things like hypothermia, freezing to death, or a heart attack.

"Wintry mix"

Many factors influence the form precipitation will take, and atmospheric temperatures are influential as well as ground conditions. Sometimes, near the rain/snow interface a region of sleet or freezing rain will occur. It is difficult to predict what form this precipitation will take, and it may alternate between rain and snow. Therefore, weather forecasters just predict a "wintry mix". Usually, this type of precipitation occurs at temperatures between -2°C and 2°C (28°F–36°F).

Freezing rain and ice storms

Freezing rain storms are one of the most dangerous types of winter storm. They typically occur when a layer of warm air hovers over a region, but the ambient temperature is near 0°C (32°F), and the ground temperature is sub-freezing. A storm in which only roads freeze is a "freezing rain storm"; one resulting in widespread icing of plants and infrastructure is an "ice storm".

While a 10 cm (4 in.) snowstorm is somewhat manageable, by the standards of the northern United States and Canada, a comparable 1 cm (0.4 in.) ice storm will paralyze a region: driving becomes extremely hazardous, telephone and power lines are damaged, and crops may be ruined. Because they do not require extreme cold, ice storms often occur in warm temperature climates (such as the southern United States) as well as cooler ones. Ice storms in Florida will often destroy entire orange crops.

Notable ice storms include an El Niño-related Ice Storm of January 1998, that affected upstate New York and much of eastern Canada, including Montreal. Three million people lost power, some for as long as six weeks. One-third of the trees in Montreal's Mount Royal park were damaged, as well as a large proportion of the sugar-producing maple trees. The amount of economic damage caused by the storm has been estimated at dollar|Can. $" target="_blank" >^*3 billion.

The Ice Storm of December 2002 in North Carolina resulted in massive power loss throughout much of the state, and property damage due to falling trees. Snow and icy conditions are rare in North Carolina, even in the winter (except in the mountainous areas of the extreme western part of the state).

The Ice Storm of December 2005 was a damaging winter storm that produced extensive ice damage in a large portion of the Southern United States on December 14 to 16. It led to widespread power outages and at least 7 deaths.

Arctic cyclones

The largest snowstorms form around polar low-pressure systems and are known as arctic cyclones. In other cases, similar storms can form around high-pressure systems and create anticyclonic storms.

Gourt Home::Gourt :: Winter storm

Snowstorms

Secondary dangers

"Wintry mix"

Freezing rain and ice storms

Arctic cyclones

See also