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Typhoons

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Typhoon Megi
(Earth Science Make it Relevant) Typhoons are mature tropical cyclones that are created in the northwestern part of the Pacific Ocean. Now, a tropical cyclone is characterized as numerous thunderstorms that contain heavy rain showers and high-speed winds. They develop over large, warm bodies of water and loose their strength when moving overland due to friction from the structures on the surface. Also, the warm water gives the typhoon the energy it needs to be powerful and without the water its energy decreases. Typhoon Megi (Korean for, “catfish”) was a powerful tropical rainstorm that devastated the west Pacific region. Megi was a high-set, extremely cold (220 Kelvin/-63 degrees Fahrenheit) typhoon that made a huge impact on various regions (National Oceanic and Atmospheric Administration [NOAA] 2010). Hurricanes are considered the greatest storms on Earth, and believe it or not, a hurricane is also a typhoon and a cyclone. Hurricane is derived from Huracan, referring to a Carib god of evil. Usually hurricanes form between latitudes of five and twenty degrees over tropical oceans, except the South Atlantic and eastern South Pacific. The North Pacific has the greatest amount of storms. In the western Pacific, hurricanes are called “typhoons,” and in the Indian Ocean they are referred to as “cyclones.” A hurricane has wind speeds of seventy four miles per hour and a round circulatory motion. Mature hurricanes average three hundred and seventy five miles per hour across, while their diameter ranges from sixty miles up to nine hundred and thirty miles wide. An extreme pressure rise produces the fast, inward-spiraling winds of a hurricane. As more air moves towards the center of the storm, the velocity increases. The surface air is warm and moist as it approaches the center of the storm. From there it turns upward and soars up in a ring of

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