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The dynamics of the tropical upwelling branch of the stratospheric Brewer-Dobson circulation are examined, with a particular focus on the role of the middle-atmosphere Hadley circulation. Upwelling is examined in terms of both the diabatic circulation and Lagrangian trajectories using a zonally symmetric balance model. The behavior of the wave-driven circulation in the presence of angular momentum redistribution by the Hadley circulation is also considered. The results of the zonally symmetricdoi:10.1175/1520-0469(2001)058<3097:mftuit>2.0.co;2 fatcat:xh6zfs7uibepxlhxnhznnqtejy