The low pressure conditions which once prevailed over north-western India get transferred to the centre of Bay of Bengal by early November. This shift of the low pressure area is far south. The period is associated with occurrence of cyclonic depressions which originate over the Andaman area. These tropical cyclones are often very destructive.
The thickly populated deltas of the Godavari, Krishna and Kaveri are their reflected argets. No year is ever found disaster free. Occasionally, these tropical cyclones visit Sundarbans and Bangladesh too. Bulk of the rainfall of the Coromandel Coast is derived from depressions and cyclones.
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