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Examine This Report on cyclone

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The passage of the tropical cyclone above the ocean results in the higher layers of the ocean to chill significantly, a method often called upweling,[62] which could negatively influence subsequent cyclone progress. This cooling is primarily due to wind-pushed mixing of cold drinking water from further while in the ocean https://finn9vpjb.thekatyblog.com/29122600/5-essential-elements-for-cyclone

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