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It is caused by a combination of strong winds driving water onshore and the lower atmospheric pressure in a tropical cyclone. In the southern hemisphere, the onshore winds occur to the left of the tropical cyclone's path.
The main causes of cyclones in the environment are well-known and documented; a small warm air mass rotating over warmer waters, picking up energy with a low-pressure center; feeding itself from the warm waters and rapidly rotating due to the Coriolis Effect, continues until the energy dissipates.
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