Simulation of recent Southern Hemisphere climate change

Nathan P. Gillett, David W. J. Thompson

Research output: Contribution to journalArticlepeer-review

496 Citations (Scopus)


Recent observations indicate that climate change over the high latitudes of the Southern Hemisphere is dominated by a strengthening of the circumpolar westerly flow that extends from the surface to the stratosphere. Here we demonstrate that the seasonality, structure, and amplitude of the observed climate trends are simulated in a state-of-the-art atmospheric model run with high vertical resolution that is forced solely by prescribed stratospheric ozone depletion. The results provide evidence that anthropogenic emissions of ozonedepleting gases have had a distinct impact on climate not only at stratospheric levels but at Earth's surface as well.
Original languageEnglish
Pages (from-to)273-275
Number of pages3
Issue number5643
Publication statusPublished - 10 Oct 2003

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