Cirkulyaciya atmosfery, obshaya
(ot lat. circulatio - vrashenie) – planetarnaya sistema vozdushnyh techenii nad zemnoi poverhnost'yu, gorizontal'nye razmery kotoroi soizmerimy s materikami i okeanami, a tolshina sostavlyaet ot neskol'kih km do desyatkov km. Peremeshenie vozdushnyh mass proishodit pod vliyaniem neodinakovogo nagrevaniya zemnoi poverhnosti na raznyh shirotah, a takzhe nad materikami i okeanami.Obshaya cirkulyaciya atmosfery opredelyaetsya zonami vysokogo atmosfernogo davleniya v pripolyarnyh oblastyah i tropicheskih shirotah i zonami nizkogo davleniya v umerennyh i ekvatorial'nyh shirotah. Peremeshenie vozdushnyh mass proishodit kak v shirotnom, tak i v meridional'nom napravleniyah. V troposfere k cirkulyacii atmosfery otnosyatsya passaty, zapadnye vozdushnye techeniya umerennyh shirot, mussony, ciklony i anticiklony.
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