Atmospheric Chemistry and Physics (Nov 2012)

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

DOI
https://doi.org/10.5194/acp-12-10033-2012
Journal volume & issue
Vol. 12, no. 21
pp. 10033 – 10050

Abstract

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HCFC-22 (CHClF<sub>2</sub>, 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.