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Typically, tropical cyclones form at least 5.0 degrees of latitude north and south of the equator, or at least 300 nautical miles from the equator. Within 5 degrees of the equator, tropical cyclogenesis is uncommon despite the presence of sufficiently warm sea surface temperatures and generally low wind shear, as a result of the lack of a strong Coriolis force, which causes cyclones to spin. On rare occasions, tropical cyclones can develop within 5° of the equator, most commonly in the northwestern Pacific Ocean.
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