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Inorganic chlorine variability in the Antarctic vortex and implications for ozone recovery

  • Published:2014-12-18 Issue:24 Volume:119 Page:14,098-14,109
  • ISSN:2169-897X
  • Container-title:Journal of Geophysical Research: Atmospheres
  • language:en
  • Short-container-title:J. Geophys. Res. Atmos.

Author:

Strahan S. E.12,Douglass A. R.2,Newman P. A.2,Steenrod S. D.12

Affiliation:

1. Goddard Earth Sciences Technology and Research; Universities Space Research Association; Columbia Maryland USA

2. NASA Goddard Space Flight Center; Greenbelt Maryland USA

Funder

NASA Modeling, Analysis, and Prediction Program

NASA Atmospheric Composition Modeling and Analysis Program

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Reference39 articles.

1. Unusual stratospheric transport and mixing during the 2002 Antarctic winter;Allen;Geophys. Res. Lett.,2003

2. Indicators of Antarctic ozone depletion;Bodeker;Atmos. Chem. Phys.,2005

3. On the evaluation of halocarbon radiative forcing and global warming potentials;Daniel;J. Geophys. Res.,1995

4. Nitrous oxide and sulfur hexafluoride [in 'State of the Climate in 2008'];Elkins;Bull. Am. Meteorol. Soc.,2009

5. Large losses of total ozone in Antarctica reveal seasonal ClOx/NOx interaction;Farman;Nature,1985

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