Most Indian ocean cyclones are caused by a combination of warm sea surface temperatures, atmospheric instability, and favorable wind shear conditions. Typically occurring between April and December, these storms develop when warm ocean waters provide the necessary energy and moisture. Additionally, the monsoon season and the presence of the Intertropical Convergence Zone (ITCZ) play significant roles in cyclone formation. The region's unique geography and climatic patterns further influence the intensity and frequency of these cyclones.
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