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Atmospheric histories and global emissions of halons H-1211 (CBrClF2), H-1301 (CBrF3), and H-2402 (CBrF2CBrF2)

  • Martin K. Vollmer
  • , Jens Mühle
  • , Cathy M. Trudinger
  • , Matthew Rigby
  • , Stephen A. Montzka
  • , Christina M. Harth
  • , Benjamin R. Miller
  • , Stephan Henne
  • , Paul B. Krummel
  • , Bradley D. Hall
  • , Dickon Young
  • , Jooil Kim
  • , Jgor Arduini
  • , Angelina Wenger
  • , Bo Yao
  • , Stefan Reimann
  • , Simon O’Doherty
  • , Michela Maione
  • , David M. Etheridge
  • , Shanlan Li
  • Daniel P. Verdonik, Sunyoung Park, Geoff Dutton, L. Paul Steele, Chris R. Lunder, Tae Siek Rhee, Ove Hermansen, Norbert Schmidbauer, Ray H.J. Wang, Matthias Hill, Peter K. Salameh, Ray L. Langenfelds, Lingxi Zhou, Thomas Blunier, Jakob Schwander, James W. Elkins, James H. Butler, Peter G. Simmonds, Ray F. Weiss, Ronald G. Prinn, Paul J. Fraser
  • Swiss Federal Laboratories for Materials Science and Technology (Empa)
  • University of California at San Diego
  • CSIRO
  • University of Bristol
  • National Oceanic and Atmospheric Administration
  • University of Colorado Boulder
  • University of Urbino
  • National Research Council of Italy
  • China Meteorological Administration
  • Kyungpook National University
  • Jensen Hughes
  • Norwegian Institute for Air Research
  • Korea Polar Research Institute
  • Georgia Institute of Technology
  • University of Copenhagen
  • University of Bern
  • Massachusetts Institute of Technology

Research output: Contribution to journalArticlepeer-review

28 Scopus citations

Abstract

We report ground-based atmospheric measurements and emission estimates for the halons H-1211 (CBrClF2), H-1301 (CBrF3), and H-2402 (CBrF2CBrF2) from the AGAGE (Advanced Global Atmospheric Gases Experiment) and the National Oceanic and Atmospheric Administration global networks. We also include results from archived air samples in canisters and from polar firn in both hemispheres, thereby deriving an atmospheric record of nearly nine decades (1930s to present). All three halons were absent from the atmosphere until ~1970, when their atmospheric burdens started to increase rapidly. In recent years H-1211 and H-2402 mole fractions have been declining, but H-1301 has continued to grow. High-frequency observations show continuing emissions of H-1211 and H-1301 near most AGAGE sites. For H-2402 the only emissions detected were derived from the region surrounding the Sea of Japan/East Sea. Based on our observations, we derive global emissions using two different inversion approaches. Emissions for H-1211 declined from a peak of 11 kt yr-1 (late 1990s) to 3.9 kt yr-1 at the end of our record (mean of 2013-2015), for H-1301 from 5.4 kt yr-1 (late 1980s) to 1.6 kt yr-1, and for H-2402 from 1.8 kt yr-1 (late 1980s) to 0.38 kt yr-1. Yearly summed halon emissions have decreased substantially; nevertheless, since 2000 they have accounted for ~30% of the emissions of all major anthropogenic ozone depletion substances, when weighted by ozone depletion potentials.

Original languageEnglish
Pages (from-to)3663-3686
Number of pages24
JournalJournal of Geophysical Research
Volume121
Issue number7
DOIs
StatePublished - 2016

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 12 - Responsible Consumption and Production
    SDG 12 Responsible Consumption and Production

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