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Cyclone - An Overview

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The passage of the tropical cyclone more than the ocean brings about the higher layers in the ocean to chill significantly, a procedure generally known as upweling,[sixty two] which can negatively affect subsequent cyclone growth. This cooling is generally brought on by wind-driven mixing of chilly drinking water from further https://paxton9hnr4.weblogco.com/29981598/cyclone-no-further-a-mystery

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