structure of a cyclone
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Tropical Cyclone Structure. The main parts of a tropical cyclone are the rainbands, the eye, and the eyewall. Air spirals in toward the center in a counter-clockwise pattern in the northern hemisphere (clockwise in the southern hemisphere), and out the top in the opposite direction.
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The centre of a cyclone is a calm area. It is called the eye of the storm. A large cyclone is a violently rotating mass of air in the atmosphere, 10to15km high. The diameter of the eye varies from 10 to 30 km. It is a region free of clouds and has light winds. Around his calm and clear eye, there is a cloud region of about 150 km in size. In this region there are high-speed winds (150-250 km/h) and thick cloud ☁️ with heavy rain. Away from this region the wind speed gradually decreases. The formation of a cyclone is a very complex process.
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