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New Step by Step Map For cyclone

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The passage of a tropical cyclone around the ocean causes the higher levels with the ocean to chill considerably, a approach often known as upweling,[62] which might negatively affect subsequent cyclone enhancement. This cooling is primarily attributable to wind-driven mixing of chilly h2o from further in the ocean with the https://bigwin31853.blogvivi.com/30473700/the-5-second-trick-for-cyclone

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