Describe the structure of a cyclone with a model.
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The centre of 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 around 10 to 15 km high. The diameter of the eye varies from 10 to 30 km. It is a cloud free region with a mixture of light wing in it. Around this calm and clear eye, there is a cloud region of about 150km in size. In this region there are high-speed winds(150-250km/h) and thick clouds 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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The structure of a typhoon is as follows:
- The phase is defined using the asymmetry parameters of the thickness relative to the storm movement and the vertical output of the horizontal gradient.
- The life cycle of a hurricane can be analysed within this phase space, providing a deeper understanding of the emergence of cyclone structure.
- Targeted classification of the storm phase is possible, which includes the basic structural definition of tropical, extra tropical, and hybrid cyclones into continuous.
- The main components of tropical cyclones are rain gloves, eye, and eye wall.
- The wind rotates toward the canter in a pattern opposite the clock in the north of the equator (clockwise in the south equator), and rises upward in the opposite direction.
- In the middle of a storm, the air sinks, creating a cloudless "eye".
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