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1. 60° to 65° N&S2. Dynamically induced due to Coriolis force3. Ascent of air caused by convergence of polar easterlies and westerlies; also by Earth's rotation

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1. 1. 60° to 65° N&S
2. Dynamically induced due to Coriolis force
3. Ascent of air caused by convergence of polar easterlies and westerlies; also by Earth's rotation





 
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