When Does Freezing Rain Become An Ice Storm?

The author could have easily used plain words to tell the story, but he did not. To describe the storm, Heynen uses the word “splintering.” Most people know that splinters sometime hurt. This gives the illusion that the ice was hitting them in little sharp pieces. Heynen also uses “gelatin whites.” Gelatin means translucent so Heynen says that it is see through whites. Last, he uses “clinging” to show how the ice is sticking to their skin and is not coming off. As a result, Heynen uses interesting word choice to describe certain parts of the

Mother Nature can form many powerful storms, such as hurricanes, blizzards, typhoons, and cyclones. However, the two storms that are significant to the New England area are hurricanes and blizzards due to their extremely powerful type of weather. Hurricanes and blizzards can be catastrophic and cause excessive damage, however under different conditions. Blizzards involve large mass amounts of snow covering a wide area, while a hurricane involves excessive rain and tremendous winds. Both storms are quite different; however, there are a few similarities. A hurricane is characterized by thunderstorms, strong winds, and heavy rains. A blizzard is a storm with dry, strong winds, and intense cold. Blizzards and hurricanes are two natural phenomena that make an interesting comparison and contrast in how they are formed and how disastrous they can be.

Frost forms when there is enough moisture in the air and the ground is cold to

Frontal rainfall occurs when warm air meets cold air,the warm air is forced over the cold air ,When the air meets the warm air it is cooled and water vapour condenses,clouds form and the rainfall

According to the forecasters only about 12 inches of actual snow fell. Their assumptions on the rest of the snow is it blew from Lake Erie to the sounding locations. Snow was recorded in areas up to 100 inches deep (usatoday.com). This varied some from location to location but all the surrounding areas were hit hard. Most areas only see this amount over weeks or months. Most of the snow accumulated in several hours up to a few days. Never had snow crews seen this much in such a short period of time. Due to the large amount of snow it left many motorists stranded. A large portion of the death tolls from this storm came from people stranded in their vehicle. Once there vehicles were stuck there only means of heat was from the vehicle running. In some cases the vehicles ran out of gas and in some they broke

As with the huge snowstorm of December 1974 another even more powerful (in terms of intensity/extent) storm is of strong interest to all meteorologists who have studied winter storms in the Great Lakes. This storm is also of interest and remembrance to many longtime residents of the Great Lakes, the Upper Ohio Valley and Ontario, Canada who had to deal with winter's full fury late in January of 1978. In addition, the storm certainly casts many memories for those of us who were on duty and worked during the storm...while being in awe of the development and subsequent immense strength of this great monster. With the 30th anniversary of this Great Blizzard at hand, it is worth taking a step back in time to re-live this monumental example of nature's fury.

Below freezing air is used to make snow and snowflakes. Moisture from lakes and oceans to form clouds.warm, rising air to form precipitation.

These temperatures result in large snow storms dumping eight to sixteen inches of snow at a time. Even with such large snowfall, most schools in major cities don’t shut down for the day. Instead classes are delayed til the middle of the morning, allowing for snow plows to get out and clear the roads. The only schools that normally close during snow storms are those located in the most rural locations of the state. Rainfall throughout the year averages about four inches a month, just falling in different forms. Summer months usually produce warm temperatures in the seventies, warming water temperatures up enough to go to coastal beaches. New York is often hit by the remains of hurricanes that have traveled up the east coast. These dump several inches of water on the state at a time. New York doesn’t have the standard tornado thought of by Oklahomans, but with the right mixture over the Great Lakes region, the weather often produces water spouts. These spouts are usually harmless forms of tornadoes, with wind speeds reaching sixty miles an hour, and often die out quickly. While the far northern parts of the state can be different, the state of New York as a whole has a fairly consistent climate from year to year.

After a careful overview of the story, the readers understands that the author point is that in some situations, people should do the nice thing and sacrifice themselves to help others. In the story, “What Happened During the Ice storm” the author uses a mysterious, bittersweet tone, “They stood over the pheasants, turning their own heads, looking at each other each expecting the other to do something” (Heynen 1). The author uses this line to show that any other person would not even stop to think; that any other person would immediately attack. However, putting these lines in the story makes the reader notice how the boys took the time to stop and think

“Weather is just weather. It’s never just rain” (44). If a setting in a story involves rain it’s not because outside was hot and all the water evaporated into the clouds and couldn’t hold anymore so it started to pour. I mean who would ever think of such a thing? Usually when a story contains raining it can mean the character is being “purified” or transformed. However with rain comes mud, which can cause the character to be more tainted then before. Rain is also associated with spring, which is a period of rebuilding and all the more imperatively, trust. Mist can include the wretchedness element, additionally disarray among characters and circumstances. Snow is generally as critical and negating as downpour. It can be spotless, welcoming, lively, or even warm (like a protecting blanket).However it can likewise be stark, serious, cold choking, and even grimy. The Great Gatsby, by F. Scott Fitzgerald, Gatsby and Daisy's get-together starts amidst a deluge which

Ice starts as water that has a temperature of any degree above thirty-two degrees Fahrenheit. Before water technically becomes water, which is the name of the liquid state, it starts as a gas called water vapor. After water vapor condenses because of a loss of energy, it is then in liquid phase of H2O, called water, which can then be broken down in the smallest unit; atoms.

In the article " Snow Day," by Tabitha Walker, she explains the ways of how the snowflake's process can be complete. Precipitation only falls as snow when the air temperature is 32 degrees Fahrenheit or below. However, if the air is 15 degree Fahrenheit or below, the snowflakes might not generate because they need moisture to generate. When the temperature is freezing, the more heavy snow will fall. If you want bigger snowflakes then you need more moisture in the air, if you want smaller snowflakes you need less moisture and more freezing temperature.

In Kansas City, April 2001 there was a hail storm that costed a total of $2 billion to fix the damage that was done to cars, roofs, buildings and crops. On the other hand there are different sizes of hail that can determine how much damage that can be done. Small hail is the size of a pea and can destroy a vegetable garden to shreds while large hail can either be the size of a tennis ball or bigger and can destroy rooftops, cars and windows. The reason why hail is dangerous is because they are clumps of ice that are formed by thunder clouds. Thunder clouds create hail by the strong up draft that carries the winds precipitation to the very top. Eventually the ice gets heavy enough and falls at sub-freezing temperatures and collects moisture

Blizzards often form in the northern plains, surprisingly. Even though there is more snow in the northeast, it is often too wet and heavy from the East Coast that they can’t be picked up by wind. Therefore, they would not be counted as blizzards, which require snow and high wind speeds. The northern plains are perfect for blizzards, because firstly, the flat terrain allows the wind speed to reach 35 mph or more, second, the cold and dry temperature allows the snow to be thrown around. Third, Alberta Clipper storm systems - the fast moving low pressure area which generally affects the northwest areas - usually last more than 3 hours, making them count as

They are known as rime and clear ice, and a mixture of the two is not uncommon. For rime ice to form, an aircraft needs to fly through an area of tiny super-cooled liquid drops. This super-cooled liquid is actually suspended in the cloud cover at temperatures already below freezing. Once the aircraft surface plows through this moisture, the drops are disrupted immediately adhere to and freeze before spreading out over the entire surface. This forms a rough and cloudy-white layer of ice known as rime. Even though the rime surface is rough and creates an airflow disturbance, it is lighter and easier to remove by deicing equipment than clear ice. For clear ice to form, larger sized super-cooled drops would need to be encountered. These larger droplets spread out over the surface and airfoils before freezing. This allows for the build-up of a clear, hard and slick layer of ice on the surface (Ahrens, 2009).