Articles | Volume 16, issue 16
https://doi.org/10.5194/acp-16-10725-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-16-10725-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
20 years of ClO measurements in the Antarctic lower stratosphere
Gerald E. Nedoluha
CORRESPONDING AUTHOR
Naval Research Laboratory, Washington, D.C., USA
Brian J. Connor
BC Scientific Consulting LLC, Stony Brook, NY, USA
Thomas Mooney
BC Scientific Consulting LLC, Stony Brook, NY, USA
James W. Barrett
Stony Brook University, Stony Brook, NY, USA
Alan Parrish
Department of Astronomy, University of Massachusetts, Amherst, MA, USA
R. Michael Gomez
Naval Research Laboratory, Washington, D.C., USA
Ian Boyd
BC Scientific Consulting LLC, Stony Brook, NY, USA
Douglas R. Allen
Naval Research Laboratory, Washington, D.C., USA
Michael Kotkamp
National Institute of Water and Atmospheric Research, Lauder, New
Zealand
Stefanie Kremser
Bodeker Scientific, Alexandra, New Zealand
Terry Deshler
Department of Atmospheric Science, University of Wyoming, Laramie, WY,
USA
Paul Newman
NASA Goddard Space Flight Center, Greenbelt, MD, USA
Michelle L. Santee
Jet Propulsion Laboratory, California Institute of Technology,
Pasadena, CA, USA
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Cited
8 citations as recorded by crossref.
- Upper stratospheric ClO and HOCl trends (2005–2020): Aura Microwave Limb Sounder and model results L. Froidevaux et al. 10.5194/acp-22-4779-2022
- The Network for the Detection of Atmospheric Composition Change (NDACC): history, status and perspectives M. De Mazière et al. 10.5194/acp-18-4935-2018
- The impact of dehydration and extremely low HCl values in the Antarctic stratospheric vortex in mid-winter on ozone loss in spring Y. Zhang-Liu et al. 10.5194/acp-24-12557-2024
- Decline in Antarctic Ozone Depletion and Lower Stratospheric Chlorine Determined From Aura Microwave Limb Sounder Observations S. Strahan & A. Douglass 10.1002/2017GL074830
- The Antarctic ozone hole during 2020 A. Klekociuk et al. 10.1071/ES21015
- Strato-mesospheric carbon monoxide profiles above Kiruna, Sweden (67.8 ° N, 20.4 ° E), since 2008 N. Ryan et al. 10.5194/essd-9-77-2017
- Evolution of observed ozone, trace gases, and meteorological variables over Arrival Heights, Antarctica (77.8°S, 166.7°E) during the 2019 Antarctic stratospheric sudden warming D. Smale et al. 10.1080/16000889.2021.1933783
- The Antarctic ozone hole during 2018 and 2019 A. Klekociuk et al. 10.1071/ES20010
8 citations as recorded by crossref.
- Upper stratospheric ClO and HOCl trends (2005–2020): Aura Microwave Limb Sounder and model results L. Froidevaux et al. 10.5194/acp-22-4779-2022
- The Network for the Detection of Atmospheric Composition Change (NDACC): history, status and perspectives M. De Mazière et al. 10.5194/acp-18-4935-2018
- The impact of dehydration and extremely low HCl values in the Antarctic stratospheric vortex in mid-winter on ozone loss in spring Y. Zhang-Liu et al. 10.5194/acp-24-12557-2024
- Decline in Antarctic Ozone Depletion and Lower Stratospheric Chlorine Determined From Aura Microwave Limb Sounder Observations S. Strahan & A. Douglass 10.1002/2017GL074830
- The Antarctic ozone hole during 2020 A. Klekociuk et al. 10.1071/ES21015
- Strato-mesospheric carbon monoxide profiles above Kiruna, Sweden (67.8 ° N, 20.4 ° E), since 2008 N. Ryan et al. 10.5194/essd-9-77-2017
- Evolution of observed ozone, trace gases, and meteorological variables over Arrival Heights, Antarctica (77.8°S, 166.7°E) during the 2019 Antarctic stratospheric sudden warming D. Smale et al. 10.1080/16000889.2021.1933783
- The Antarctic ozone hole during 2018 and 2019 A. Klekociuk et al. 10.1071/ES20010
Saved (preprint)
Latest update: 23 Nov 2024
Short summary
Chlorine monoxide (ClO) is central to the formation of the springtime Antarctic ozone hole since it is the catalytic agent in the most important ozone-depleting chemical cycle. We present 20 years of measurements of ClO from the Chlorine monOxide Experiment at Scott Base, Antarctica, and 12 years of measurements from the Aura Microwave Limb Sounder to show that the trends in ClO during the ozone hole season are consistent with changes in stratospheric chlorine observed elsewhere.
Chlorine monoxide (ClO) is central to the formation of the springtime Antarctic ozone hole since...
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