Tropical cyclones form when warm, moist air rises and condenses into clouds. This process releases heat, which warms the surrounding air and causes it to rise as well. As the warm air continues to rise, it forms a rotating system of clouds and winds. This rotating system can grow in size and intensity, eventually forming a tropical cyclone.
For a tropical cyclone to form, certain conditions must be met, including:
    1. Warm sea surface temperatures of at least 26.5°C (79.7°F).
    2. High humidity in the lower atmosphere.
    3. Weak vertical wind shear (change in wind direction and speed with height).
    4. Convergence of moist air near the surface.
These conditions must come together in a specific way, with the right balance of temperature, moisture, and wind, in order to create a tropical cyclone. Once formed, the system can continue to grow and intensify as long as these conditions persist.
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