ðə ɹˈaɪzɪŋ ˈɛɹ, ænd kɑːndɛnsˈeɪʃən, pɹədˈuːsᵻz sˈɜːkjʊlətˌoːɹi wˈɪndz ðæt ɑːɹ pɹəpˈɛld baɪ ðə kˌɔːɹɪˈoʊliz fˈoːɹs, wˌɪtʃ wˈɪp ˌʌp wˈeɪvz ænd ˈɪŋkɹiːs ðɪ ɐmˈaʊnt ʌv wˈɔːɹm mˈɔɪst ˈɛɹ ðæt pˈaʊɚz ðə sˈaɪkloʊn.
The rising air, and condensation, produces circulatory winds that are propelled by the Coriolis force, which whip up waves and increase the amount of warm moist air that powers the cyclone.