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A large ozone-circulation feedback and its implications for global warming assessments

Author

Listed:
  • Peer J. Nowack

    (Centre for Atmospheric Science, University of Cambridge)

  • N. Luke Abraham

    (Centre for Atmospheric Science, University of Cambridge
    National Centre for Atmospheric Science)

  • Amanda C. Maycock

    (Centre for Atmospheric Science, University of Cambridge
    National Centre for Atmospheric Science)

  • Peter Braesicke

    (Centre for Atmospheric Science, University of Cambridge
    National Centre for Atmospheric Science
    Present addresses: Karlsruhe Institute of Technology, IMK-ASF, 76344 Eggenstein-Leopoldshafen, Germany (P.B.); Centre for Ocean and Atmospheric Sciences, University of East Anglia, Norwich NR4 7TJ, UK (M.M.J.).)

  • Jonathan M. Gregory

    (National Centre for Atmospheric Science
    University of Reading
    Met Office Hadley Centre, Met Office)

  • Manoj M. Joshi

    (National Centre for Atmospheric Science
    University of Reading
    Present addresses: Karlsruhe Institute of Technology, IMK-ASF, 76344 Eggenstein-Leopoldshafen, Germany (P.B.); Centre for Ocean and Atmospheric Sciences, University of East Anglia, Norwich NR4 7TJ, UK (M.M.J.).)

  • Annette Osprey

    (National Centre for Atmospheric Science
    University of Reading)

  • John A. Pyle

    (Centre for Atmospheric Science, University of Cambridge
    National Centre for Atmospheric Science)

Abstract

Climate models include many processes that may be simplified to save computational time. This work shows that model representation of upper atmosphere ozone can impact on the projected climate sensitivity.

Suggested Citation

  • Peer J. Nowack & N. Luke Abraham & Amanda C. Maycock & Peter Braesicke & Jonathan M. Gregory & Manoj M. Joshi & Annette Osprey & John A. Pyle, 2015. "A large ozone-circulation feedback and its implications for global warming assessments," Nature Climate Change, Nature, vol. 5(1), pages 41-45, January.
    • Handle: RePEc:nat:natcli:v:5:y:2015:i:1:d:10.1038_nclimate2451
    DOI: 10.1038/nclimate2451
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