Climate

Effect of zonal asymmetries in stratospheric ozone on simulated Southern Hemisphere climate trends

  1. D. W. Waugh1,
  2. L. Oman1,
  3. P. A. Newman2,
  4. R. S. Stolarski2,
  5. S. Pawson3,
  6. J. E. Nielsen3,
  7. J. Perlwitz4

Article first published online: 22 SEP 2009

DOI: 10.1029/2009GL040419

Issue

Geophysical Research Letters

Geophysical Research Letters

Volume 36, Issue 18, September 2009

Additional Information

How to Cite

Waugh, D. W., L. Oman, P. A. Newman, R. S. Stolarski, S. Pawson, J. E. Nielsen, and J. Perlwitz (2009), Effect of zonal asymmetries in stratospheric ozone on simulated Southern Hemisphere climate trends, Geophys. Res. Lett., 36, L18701, doi:10.1029/2009GL040419.

Author Information

  1. 1

    Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, Maryland, USA

  2. 2

    Atmospheric Chemistry and Dynamics Branch, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

  3. 3

    Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

  4. 4

    Cooperative Institute for Research in Environmental Sciences, University of Colorado, NOAA, Boulder, Colorado, USA

Publication History

  1. Issue published online: 22 SEP 2009
  2. Article first published online: 22 SEP 2009
  3. Manuscript Accepted: 27 AUG 2009
  4. Manuscript Revised: 21 AUG 2009
  5. Manuscript Received: 6 AUG 2009

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Keywords:

  • ozone;
  • climate

[1] Stratospheric ozone is represented in most climate models by prescribing zonal-mean fields. We examine the impact of this on Southern Hemisphere (SH) trends using a chemistry climate model (CCM): multi-decadal simulations with interactive stratospheric chemistry are compared with parallel simulations using the same model in which the zonal-mean ozone is prescribed. Prescribing zonal-mean ozone results in a warmer Antarctic stratosphere when there is a large ozone hole, with much smaller differences at other times. As a consequence, Antarctic temperature trends for 1960 to 2000 and 2000 to 2050 in the CCM are underestimated when zonal-mean ozone is prescribed. The impacts of stratospheric changes on the tropospheric circulation (i.e., summertime trends in the SH annular mode) are also underestimated. This shows that SH trends related to ozone depletion and recovery are underestimated when interactions between stratospheric ozone and climate are approximated by an imposed zonal-mean ozone field.

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