Use BookMyEssay:Tropical Cyclone Assignment Help

Also known as a hurricane or typhoon, a tropical cyclone is acknowledged as a serious circular storm. It gets characterized by high winds, heavy rains, and low atmospheric pressure, and originates over tropical oceans. 

Characteristics of Tropical Cyclone

Tropical Cyclone get energy from the surface of the sea and they maintain their strength when they hover over warm water. The winds of a tropical cyclone exceed 119 kilometers or 74 miles every hour. In an extreme case, winds exceed 240 kilometers or 150 miles per hour too.

The gusts might cross 200 miles or 320 kilometers per hour. These strong winds remain accompanied by torrential rains besides a distressing phenomenon that is called the storm surge. This is an elevation of the surface of the sea that is capable of reaching 20 feet or 6 meters above normal levels. As cyclones are a combination of water and high winds, they become a severe danger for a coastal area present in subtropical and tropical areas. Every year, in Northern Hemisphere, at the time of summer months (July to September), and in Southern Hemisphere, (January to March) cyclones strike.

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What causes a Tropical Cyclone?

Based on research, it has been discovered that a tropical cyclone is caused by escalating temperatures of the sea surface. This report recommended that coastal buildings, bridges, and roads are required to build for withstanding heavy rainfall, high wind speeds, and possible storms. It will prevent damage to the costly infrastructure.

How do Tropical Cyclone Get Formed?

A tropical cyclone represents another instance of the interaction of air and sea, and these storm systems are called hurricanes. Tropical Cyclone might last from some hours to even a couple of weeks. The average lifetime of a tropical cyclone is 6 days. An ocean becomes a tropical cyclone’s source of energy by the water evaporation and direct heat transfer.

After this, the water is condensed in a storm system, so, releases talent heat energy. If Tropical Cyclone move over land, then this energy is depleted. In this situation, the wind circulation too becomes weak. These kinds of storms are phenomena of a tropical ocean. Tropical Cyclone originate in a couple of distinct latitude zones, between 4^o and 35^o N and 4^o and 22^o S. However, Tropical Cyclone remain absent in an equatorial zone that is between 4^o S and 4^o N. The majority of Tropical Cyclone get created on the ITCZ (intertropical convergence zone).

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