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New Step by Step Map For cyclone

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The passage of the tropical cyclone around the ocean results in the higher levels in the ocean to cool substantially, a process known as upweling,[sixty two] that may negatively impact subsequent cyclone growth. This cooling is largely attributable to wind-driven mixing of chilly h2o from deeper within the ocean with https://trevorgge83.blogchaat.com/29942846/5-simple-statements-about-cyclone-explained

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