Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.

Site Tools

  • AAAS
  • Subscribe
  • Feedback

Site Search

Search Advanced

Science 10 October 2003:
Vol. 302. no. 5643, pp. 273 - 275
DOI: 10.1126/science.1087440
Prev | Table of Contents | Next

Reports

Simulation of Recent Southern Hemisphere Climate Change

Nathan P. Gillett1* and David W. J. Thompson2

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.

1 School of Earth and Ocean Sciences, University of Victoria, Post Office Box 3055, Victoria, BC V8W3P6, Canada.
2 Department of Atmospheric Science, Foothills Campus, Colorado State University, Fort Collins, CO 80523, USA.

* To whom correspondence should be addressed. E-mail: gillett{at}uvic.ca

Read the Full Text


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
The Impact of Stratospheric Ozone Recovery on the Southern Hemisphere Westerly Jet.
S.-W. Son, L. M. Polvani, D. W. Waugh, H. Akiyoshi, R. Garcia, D. Kinnison, S. Pawson, E. Rozanov, T. G. Shepherd, and K. Shibata (2008)
Science 320, 1486-1489
   Abstract »    Full Text »    PDF »


ADVERTISEMENT
Click Me!

ADVERTISEMENT
Click Me!

To Advertise     Find Products

Science. ISSN 0036-8075 (print), 1095-9203 (online)