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Recent Northern Hemisphere stratospheric HCl increase due to atmospheric circulation changes

Author

Listed:
  • E. Mahieu

    (Institute of Astrophysics and Geophysics, University of Liège, Liège 4000, Belgium)

  • M. P. Chipperfield

    (National Centre for Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK)

  • J. Notholt

    (University of Bremen, Bremen 28334, Germany)

  • T. Reddmann

    (Karlsruhe Institute of Technology (KIT), Institute for Meteorology and Climate Research (IMK-ASF), Karlsruhe 76021, Germany)

  • J. Anderson

    (Hampton University)

  • P. F. Bernath

    (Old Dominion University
    University of York, York YO10 5DD, UK
    University of Waterloo, Waterloo, Ontario N2L 3G1, Canada)

  • T. Blumenstock

    (Karlsruhe Institute of Technology (KIT), Institute for Meteorology and Climate Research (IMK-ASF), Karlsruhe 76021, Germany)

  • M. T. Coffey

    (National Center for Atmospheric Research)

  • S. S. Dhomse

    (National Centre for Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK)

  • W. Feng

    (National Centre for Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK)

  • B. Franco

    (Institute of Astrophysics and Geophysics, University of Liège, Liège 4000, Belgium)

  • L. Froidevaux

    (Jet Propulsion Laboratory, California Institute of Technology)

  • D. W. T. Griffith

    (School of Chemistry, University of Wollongong)

  • J. W. Hannigan

    (National Center for Atmospheric Research)

  • F. Hase

    (Karlsruhe Institute of Technology (KIT), Institute for Meteorology and Climate Research (IMK-ASF), Karlsruhe 76021, Germany)

  • R. Hossaini

    (National Centre for Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK)

  • N. B. Jones

    (School of Chemistry, University of Wollongong)

  • I. Morino

    (National Institute for Environmental Studies (NIES), Tsukuba, Ibaraki 305-8506, Japan)

  • I. Murata

    (Graduate School of Environmental Studies, Tohoku University, Sendai 980-8578, Japan)

  • H. Nakajima

    (National Institute for Environmental Studies (NIES), Tsukuba, Ibaraki 305-8506, Japan)

  • M. Palm

    (University of Bremen, Bremen 28334, Germany)

  • C. Paton-Walsh

    (School of Chemistry, University of Wollongong)

  • J. M. Russell III

    (Hampton University)

  • M. Schneider

    (Karlsruhe Institute of Technology (KIT), Institute for Meteorology and Climate Research (IMK-ASF), Karlsruhe 76021, Germany)

  • C. Servais

    (Institute of Astrophysics and Geophysics, University of Liège, Liège 4000, Belgium)

  • D. Smale

    (National Institute of Water and Atmospheric Research (NIWA), Lauder 9352, New Zealand)

  • K. A. Walker

    (University of Waterloo, Waterloo, Ontario N2L 3G1, Canada
    University of Toronto, Toronto, Ontario M5S 1A7, Canada)

Abstract

Policies have been in place since 1987 to reduce the release of chlorine atoms in the stratosphere, where they deplete ozone; here observations show that since 2007 hydrogen chloride has been increasing in the lower stratosphere of the Northern Hemisphere, an increase that is attributed to a slowdown in atmospheric circulation.

Suggested Citation

  • E. Mahieu & M. P. Chipperfield & J. Notholt & T. Reddmann & J. Anderson & P. F. Bernath & T. Blumenstock & M. T. Coffey & S. S. Dhomse & W. Feng & B. Franco & L. Froidevaux & D. W. T. Griffith & J. W., 2014. "Recent Northern Hemisphere stratospheric HCl increase due to atmospheric circulation changes," Nature, Nature, vol. 515(7525), pages 104-107, November.
  • Handle: RePEc:nat:nature:v:515:y:2014:i:7525:d:10.1038_nature13857
    DOI: 10.1038/nature13857
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