Articles | Volume 18, issue 2
https://doi.org/10.5194/acp-18-1379-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-18-1379-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Evidence for a continuous decline in lower stratospheric ozone offsetting ozone layer recovery
Physikalisch-Meteorologisches Observatorium Davos World Radiation Centre, Dorfstrasse 33, 7260 Davos Dorf, Switzerland
Institute for Atmospheric and Climate Science, Swiss Federal Institute of Technology Zurich, Universitaetstrasse 16, CHN, 8092 Zurich, Switzerland
Justin Alsing
Center for Computational Astrophysics, Flatiron Institute, 162 5th Ave, New York, NY 10010, USA
Physics Department, Blackett Laboratory, Imperial College London, SW7 2AZ, UK
Daniel J. Mortlock
Physics Department, Blackett Laboratory, Imperial College London, SW7 2AZ, UK
Department of Mathematics, Imperial College London, SW7 2AZ, UK
Department of Astronomy, Stockholm University, 106 91 Stockholm, Sweden
Johannes Staehelin
Institute for Atmospheric and Climate Science, Swiss Federal Institute of Technology Zurich, Universitaetstrasse 16, CHN, 8092 Zurich, Switzerland
Joanna D. Haigh
Physics Department, Blackett Laboratory, Imperial College London, SW7 2AZ, UK
Grantham Institute – Climate Change and the Environment, Imperial College London, SW7 2AZ, UK
Thomas Peter
Institute for Atmospheric and Climate Science, Swiss Federal Institute of Technology Zurich, Universitaetstrasse 16, CHN, 8092 Zurich, Switzerland
Fiona Tummon
Institute for Atmospheric and Climate Science, Swiss Federal Institute of Technology Zurich, Universitaetstrasse 16, CHN, 8092 Zurich, Switzerland
Rene Stübi
Federal Office of Meteorology and Climatology, MeteoSwiss, 1530 Payerne, Switzerland
Andrea Stenke
Institute for Atmospheric and Climate Science, Swiss Federal Institute of Technology Zurich, Universitaetstrasse 16, CHN, 8092 Zurich, Switzerland
John Anderson
School of Science, Hampton University, Hampton, VA, USA
Adam Bourassa
Institute of Space and Atmospheric Studies, University of Saskatchewan, Saskatoon, Canada
Sean M. Davis
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
NOAA Earth System Research Laboratory, Boulder, CO, USA
Doug Degenstein
Institute of Space and Atmospheric Studies, University of Saskatchewan, Saskatoon, Canada
Stacey Frith
NASA Goddard Space Flight Center, Greenbelt, MD, USA
Science Systems and Applications Inc., Lanham, MD, USA
Lucien Froidevaux
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA
Chris Roth
Institute of Space and Atmospheric Studies, University of Saskatchewan, Saskatoon, Canada
Viktoria Sofieva
Finnish Meteorological Institute, Earth Observation, Helsinki, Finland
School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA
Jeannette Wild
NOAA/NWS/NCEP/Climate Prediction Center, College Park, MD, USA
Innovim LLC, Greenbelt, MD, USA
Pengfei Yu
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
NOAA Earth System Research Laboratory, Boulder, CO, USA
Jerald R. Ziemke
NASA Goddard Space Flight Center, Greenbelt, MD, USA
Morgan State University, Baltimore, Maryland, USA
Eugene V. Rozanov
Physikalisch-Meteorologisches Observatorium Davos World Radiation Centre, Dorfstrasse 33, 7260 Davos Dorf, Switzerland
Institute for Atmospheric and Climate Science, Swiss Federal Institute of Technology Zurich, Universitaetstrasse 16, CHN, 8092 Zurich, Switzerland
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Short summary
Using a robust analysis, with artefact-corrected ozone data, we confirm upper stratospheric ozone is recovering following the Montreal Protocol, but that lower stratospheric ozone (50° S–50° N) has continued to decrease since 1998, and the ozone layer as a whole (60° S–60° N) may be lower today than in 1998. No change in total column ozone may be due to increasing tropospheric ozone. State-of-the-art models do not reproduce lower stratospheric ozone decreases.
Using a robust analysis, with artefact-corrected ozone data, we confirm upper stratospheric...
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