Hurricane Andrew
Hurricanes are formed by counterclockwise winds. These winds draw moisture and heat from the tropical ocean, which helps to contribute to the intense cyclone. Winds that reach and sustained 74 miles per hour (mph) or more wind are classified as a Hurricane. When a storm moves forward at about 15 mph, it releases heavy rains and accelerating winds and makes the ocean swell. They lose some intensity when they are nearing the land. As it continues to move further inland weakens, but continues it's outpouring of rain and high winds. Hurricanes are formed in the North Atlantic, Caribbean Sea, Gulf of Mexico and the Pacific Coast of Mexico. The mostly likely to happen is a hurricane striking land areas along the Gulf Coast and the southeastern coast. But hurricanes also have hit central Pennsylvania and the coast of New York, New England and New Jersey. Almost 100 million Americans are at risk from hurricanes. Over land, hurricanes weaken rapidly. Being separated from their oceanic source of energy. Plus land adds the effects of friction and that makes the circulation weakens and becomes more disorganized. Heavy rains usually continue even after the winds are much calmer. In the southeastern United States, about one-fourth
Heavy rain is another major concern. The low pressure in the middle of the storm causes a smaller part of the storm surge. The violent winds and storm surges classified Andrew as category 4 hurricane. This causes the ocean water to pile up. The currents began to change and Andrew turned toward the northwest and its speed decreased. These winds exceed 74 mph and have the ability to rip apart buildings, uproot trees and knock over power lines. The Atlantic hurricane season lasts from June through November. Most of the surge is caused by the wind. The relatively small loss of life there serves as testimony to the success and importance of coordinated programs of hurricane preparedness. Hurricane Andrew was one of the worst hurricanes in history. The last threat to worry about is a storm surge. During this weakening phase, the cyclone moved northward and then accelerated northeastward.
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