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Global and regional emission estimates for HCFC-22

  • E. Saikawa
  • , M. Rigby
  • , R. G. Prinn
  • , S. A. Montzka
  • , B. R. Miller
  • , L. J.M. Kuijpers
  • , P. J.B. Fraser
  • , M. K. Vollmer
  • , T. Saito
  • , Y. Yokouchi
  • , C. M. Harth
  • , J. Mühle
  • , R. F. Weiss
  • , P. K. Salameh
  • , J. Kim
  • , S. Li
  • , S. Park
  • , K. R. Kim
  • , D. Young
  • , S. O'Doherty
  • P. G. Simmonds, A. McCulloch, P. B. Krummel, L. P. Steele, C. Lunder, O. Hermansen, M. Maione, J. Arduini, B. Yao, L. X. Zhou, H. J. Wang, J. W. Elkins, B. Hall
  • Massachusetts Institute of Technology
  • University of Bristol
  • National Oceanic and Atmospheric Administration
  • Eindhoven University of Technology
  • CSIRO
  • Swiss Federal Laboratories for Materials Science and Technology (Empa)
  • National Institute for Environmental Studies of Japan
  • University of California at San Diego
  • Seoul National University
  • Norwegian Institute for Air Research
  • University of Urbino
  • China Meteorological Administration
  • Georgia Institute of Technology

Research output: Contribution to journalArticlepeer-review

43 Scopus citations

Abstract

HCFC-22 (CHClF2, chlorodifluoromethane) is an ozone-depleting substance (ODS) as well as a significant greenhouse gas (GHG). HCFC-22 has been used widely as a refrigerant fluid in cooling and air-conditioning equipment since the 1960s, and it has also served as a traditional substitute for some chlorofluorocarbons (CFCs) controlled under the Montreal Protocol. A low frequency record on tropospheric HCFC-22 since the late 1970s is available from measurements of the Southern Hemisphere Cape Grim Air Archive (CGAA) and a few Northern Hemisphere air samples (mostly from Trinidad Head) using the Advanced Global Atmospheric Gases Experiment (AGAGE) instrumentation and calibrations. Since the 1990s high-frequency, high-precision, in situ HCFC-22 measurements have been collected at these AGAGE stations. Since 1992, the Global Monitoring Division of the National Oceanic and Atmospheric Administration/Earth System Research Laboratory (NOAA/ESRL) has also collected flasks on a weekly basis from remote sites across the globe and analyzed them for a suite of halocarbons including HCFC-22. Additionally, since 2006 flasks have been collected approximately daily at a number of tower sites across the US and analyzed for halocarbons and other gases at NOAA. All results show an increase in the atmospheric mole fractions of HCFC-22, and recent data show a growth rate of approximately 4% per year, resulting in an increase in the background atmospheric mole fraction by a factor of 1.7 from 1995 to 2009. Using data on HCFC-22 consumption submitted to the United Nations Environment Programme (UNEP), as well as existing bottom-up emission estimates, we first create globally-gridded a priori HCFC-22 emissions over the 15 yr since 1995. We then use the three-dimensional chemical transport model, Model for Ozone and Related Chemical Tracers version 4 (MOZART v4), and a Bayesian inverse method to estimate global as well as regional annual emissions. Our inversion indicates that the global HCFC-22 emissions have an increasing trend between 1995 and 2009. We further find a surge in HCFC-22 emissions between 2005 and 2009 from developing countries in Asia-the largest emitting region including China and India. Globally, substantial emissions continue despite production and consumption being phased out in developed countries currently.

Original languageEnglish
Pages (from-to)10033-10050
Number of pages18
JournalAtmospheric Chemistry and Physics
Volume12
Issue number21
DOIs
StatePublished - 2012

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