what are the properties of air in formation of cyclone
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In a cyclone, air near the ground is pushed toward the low-pressure center of the cyclone, and then rises upward, expanding and cooling as it moves. As it cools, the rising air becomes more humid, leading to cloudiness and high humidity within the cyclone
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The formation of tropical cyclones is strongly influenced by the temperature of the underlying ocean or, more specifically, by the thermal energy available in the upper 60 metres (about 200 feet) of ocean waters. Typically, the underlying ocean should have a temperature in excess of 26 °C (about 79 °F) in this layer.
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