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New Step by Step Map For cyclone

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The passage of the tropical cyclone more than the ocean will cause the higher layers on the ocean to chill substantially, a method often called upweling,[62] which might negatively affect subsequent cyclone progress. This cooling is primarily due to wind-driven mixing of cold h2o from further inside the ocean with https://felixjj0x5.bloggerchest.com/29809371/top-cyclone-secrets

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