The winds feeding a tropical

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The winds feeding a tropical cyclone also cannot have what’s called a vertical shear, where there are different wind directions in the bottom of the atmosphere compared to the top, as that can bring the spinning system to a halt. Vertical shear over oceans, Rios-Berrios explains, is caused by wind currents that can span thousands of kilometres. They can be associated with specific weather systems or simply be part of the generate pattern of winds that travel around the world. 

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