Essay on the Hurricane Sandy Essay

September 11, 2017 General Studies

Hurricanes get their start over the warm tropical Waterss of the North Atlantic Ocean near the equator. Most hurricanes appear in late summer or early autumn. when sea temperatures are at their highest. Hurricanes merely signifier over truly warm ocean H2O of 80°F or warmer. The ambiance ( the air ) must chill off really rapidly the higher you go. Besides. the air current must be blowing in the same way and at the same velocity to coerce air upward from the ocean surface. Winds flow outward above the storm leting the air below to lift. Day after twenty-four hours the fluffy cumuli signifier atop dice updrafts.

But the cloud tops rise higher than approximately 6. 000 pess. At that tallness in the Torrid Zones. there is normally a bed of warm. dry air that acts like an unseeable ceiling or palpebra. Once in a piece. something happens in the upper air that destroys this palpebra. Scientists do non cognize how this happens at all. But when it it’s the first measure in the birth of a hurricane. With the palpebra the warm. damp air rises higher and higher. Heat energy. leased as the H2O vapour in the air condenses. As it condenses the thrusts the upper bill of exchanges to highs of 50. 000 to 60. 000 pess.

The cumuli become looming thunderheads. From outside the storm country. air moves in over the sea surface to replace the air surging upwards in the thunderheads. The air begins twirling around the storm Centre. for the same ground that the air swirls around a twister Centre. As this air swirls in over the sea surface. it soaks up more and more H2O vapour. At the storm Centre. this new supply of H2O vapour gets pulled into the thunderhead updrafts. let go ofing still more energy as the H2O vapor condenses.

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This makes the updrafts rise faster. drawing in even larger sums of air and H2O vapor from the storm’s edges. And as the updrafts speed up. air swirls faster and faster around the storm Centre. The hurricane’s wind velocity ranges from 75 stat mis to 200 stat mis per hr. The air currents of a forming hurricane tend to draw off from the Centre as the air current velocity additions. When the air currents move fast plenty. the hole develops. This hole is the grade of a full-fledge hurricane. Hurricanes rotate in a counter-clockwise way around an “eye” in the Northern Hemisphere and clockwise way in the Southern Hemisphere.

The centre of the storm or “eye” is the calmest portion. It has merely light air currents and just conditions. Within the oculus. all is unagitated and peaceable. But in the cloud wall environing the oculus. things are really different although hurricane air currents do non blow every bit fast as twister winds a hurricane is far more destructive. That’s because twister air currents cover merely a little country. normally less than a mile across-’ hurricane’s air currents may cover an country 60 stat mis broad out from the Centre of the oculus.

Another ground is tornadoes seldom last every bit long as an hr. or travel more than 100 stat mis. However. hurricane may ramp for a hebdomad or more. In that clip. it may go 10s of 1000s of stat mis over the sea and land. At sea. hurricane air currents whip up giant waves up to 20 pess high. Such moving ridges can rupture bottoms and other ocean-going ships in half. Over land. hurricane air currents can deracinate trees. blow down telephone lines and power lines. and tear chimneys off rooftops. The air is filled with lifelessly winging fragments of brick. wood. and glass.

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