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Cyclone Options

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The passage of the tropical cyclone above the ocean leads to the upper layers with the ocean to chill considerably, a method called upweling,[62] which can negatively impact subsequent cyclone progress. This cooling is principally due to wind-driven mixing of cold h2o from further inside the ocean with the warm https://spencer19ekn.mdkblog.com/35602797/top-cyclone-secrets

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