Winter Storm

5 May 2017

Winter storm From Wikipedia, the free encyclopedia Jump to: navigation, search “Snowstorm” redirects here. For other uses, see Snowstorm (disambiguation). A winter storm is an event 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 necessarily restricted to the winter season, but may occur in the late autumn and early spring as well.

Very rarely, hey may 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 (such as the 1993 Superstorm) and, in regions where temperatures are cold enough, April. Approaching winter storm in Salt Lake City. 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. citation needed] Therefore, an amount f water that would produce 0. 8 in. (2 cm. ) of rain could produce at least 8 in (20 cm) of snow. Two inches of snow (5 cm. ) 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, Dublin, Canberra, Vancouver and Las Vegas). In places where snowfall is common, such as Utica, Detroit, Denver, Ottawa, Montreal, Quebec City, Chicago, Pittsburgh, Buffalo, NY,

Winter Storm Essay Example

Toronto and Minneapolis, such small snowfalls are rarely disruptive, because winter tires are used, though snowfalls in excess of 6 in (1 5 cm) usually are. A massive snowstorm with strong winds and other conditions meeting certain criteria is known as a blizzard. A large number of heavy snowstorms, some of which were blizzards, occurred in the United States during 1888 and 1947 as well as the early and mid-1990s. The snowfall of 1947 exceeded two feet with drifts and snow piles from plowing that reached twelve feet and for months, temperatures did not rise high enough to melt the snow.

The 1993 “Superstorm” was manifest as a blizzard in most of the affected area. Large snowstorms could be quite dangerous: a 6 in. (1 5 cm. ) snowstorm will make some unplowed roads impassible, and it is possible for automobiles to get stuck in the snow. Snowstorms exceeding 12 in (30 cm) especially in southern or generally warm climates will cave the roofs of some homes and cause the loss of power. Standing dead trees can also be brought down by the weight of the snow, especially if it is wet or very dense. Even a few inches of dry snow can form drifts many feet high under windy conditions.

Dangers of Snow snow brings secondary dangers that can affect us thoroughly if we are near the place. 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. Deaths can occur from hypothermia, infections brought on by frostbite or car accidents due to slippery roads. Fires and carbon monoxide poisoning can occur after a storm causes a power outage. There are also several cases of heart attacks caused by overexertion while shovelling heavy wet snow.

Wintry showers or wintry mixes 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 oc and 2 oc (28 OF and 36 OF). Heavy showers of freezing rain 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 O oc (32 OF), and the ground temperature is sub-freezing. A storm in which only roads freeze is called a freezing rain storm; one resulting in widespread icing of plants and infrastructure is called 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) and cooler ones. Ice storms in Florida will often destroy entire orange crops. Notable ice storms include an El Niho-related North American ice storm of 1998 that affected much of eastern Canada, including Montreal and Ottawa, as well as upstate New York and part of New England. 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 amage caused by the storm has been estimated at $3 billion Canadian. 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. Except in the mountainous western part of the state, heavy snow and icy conditions are rare in North Carolina. The Ice Storm of December 2005 was another severe winter storm producing extensive ice damage across a large portion of the Southern United States on December 14 to 16. It led to power outages and at least 7 deaths.

In January 2005 Kansas had been declared a major disaster zone by President George W. Bush after an ice storm caused nearly $39 million in damages to 32 counties. Federal funds were provided to the counties during January 4-6, 2005 to aid the recovery process. [1] The January 2009 Central Plains and Midwest ice storm was a crippling and accumulation, and a few of inches of snow on top it. This brought down power lines, causing some people to go without power for a few days, to a few weeks. In some cases, some didn’t see power for a month or more. At the height of the storm, more than 2 million people were without power.

Graupel Ice crystals fall through a cloud of super-cooled droplets-minute cloud droplets that ave fallen below freezing tempature but have not frozen. The ice crystal plows into the super-cooled droplets and they immediately freeze to it. This process forms graupel, or snow pellets, as the droplet continues to accumulate on the crystal. The pellets bounce when they hit the ground. Ice pellets Main article: Ice pellets Out ahead of the passage of a warm front, falling snow may partially melt and refreeze into a frozen rain drop before it reaches the ground.

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