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Unprecedented Arctic ozone loss in 2011

  • Gloria L. Manney
  • , Michelle L. Santee
  • , Markus Rex
  • , Nathaniel J. Livesey
  • , Michael C. Pitts
  • , Pepijn Veefkind
  • , Eric R. Nash
  • , Ingo Wohltmann
  • , Ralph Lehmann
  • , Lucien Froidevaux
  • , Lamont R. Poole
  • , Mark R. Schoeberl
  • , David P. Haffner
  • , Jonathan Davies
  • , Valery Dorokhov
  • , Hartwig Gernandt
  • , Bryan Johnson
  • , Rigel Kivi
  • , Esko Kyrö
  • , Niels Larsen
  • Pieternel F. Levelt, Alexander Makshtas, C. Thomas McElroy, Hideaki Nakajima, Maria Concepcióln Parrondo, David W. Tarasick, Peter Von Der Gathen, Kaley A. Walker, Nikita S. Zinoviev
  • Jet Propulsion Laboratory, California Institute of Technology
  • New Mexico Institute of Mining and Technology
  • Alfred Wegener Institute - Helmholtz Centre for Polar and Marine Research
  • NASA Langley Research Center
  • Royal Netherlands Meteorological Institute
  • Delft University of Technology
  • Science Systems and Applications, Inc.
  • Science and Technology Corporation, Hampton
  • Université Laval and Environment and Climate Change Canada
  • Russian Federal Service for Hydrometeorology and Environmental Monitoring
  • National Oceanic and Atmospheric Administration
  • Finnish Meteorological Institute
  • Danish Meteorological Institute
  • Arctic and Antarctic Research Institute
  • National Institute for Environmental Studies of Japan
  • Instituto Nacional de Tecnica Aeroespacial
  • University of Toronto

Research output: Contribution to journalArticlepeer-review

571 Scopus citations

Abstract

Chemical ozone destruction occurs over both polar regions in local winter-spring. In the Antarctic, essentially complete removal of lower-stratospheric ozone currently results in an ozone hole every year, whereas in the Arctic, ozone loss is highly variable and has until now been much more limited. Here we demonstrate that chemical ozone destruction over the Arctic in early 2011 was-for the first time in the observational record-comparable to that in the Antarctic ozone hole. Unusually long-lasting cold conditions in the Arctic lower stratosphere led to persistent enhancement in ozone-destroying forms of chlorine and to unprecedented ozone loss, which exceeded 80 per cent over 18-20 kilometres altitude. Our results show that Arctic ozone holes are possible even with temperatures much milder than those in the Antarctic. We cannot at present predict when such severe Arctic ozone depletion may be matched or exceeded.

Original languageEnglish
Pages (from-to)469-475
Number of pages7
JournalNature
Volume478
Issue number7370
DOIs
StatePublished - Oct 27 2011

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