Global and regional emission estimates for HCFC-22

Joint Program Reprint • Journal Article
Global and regional emission estimates for HCFC-22
Saikawa, E., 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. Muhle, 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. Steel, C. Lunder, O. Hermansen, M. Maione, J. Arduini, B. Yao, L.X. Zhou, H.J. Wang, J.W. Elkins and B. Hall (2012)
Atmospheric Chemistry and Physics, 12: 10033-10050

Reprint 2012-38 [Download]

Abstract/Summary:

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.

© 2012 the authors

Citation:

Saikawa, E., 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. Muhle, 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. Steel, C. Lunder, O. Hermansen, M. Maione, J. Arduini, B. Yao, L.X. Zhou, H.J. Wang, J.W. Elkins and B. Hall (2012): Global and regional emission estimates for HCFC-22. Atmospheric Chemistry and Physics, 12: 10033-10050 (http://dx.doi.org/10.5194/acp-12-10033-2012)
  • Joint Program Reprint
  • Journal Article
Global and regional emission estimates for HCFC-22

Saikawa, E., 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. Muhle, 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. Steel, C. Lunder, O. Hermansen, M. Maione, J. Arduini, B. Yao, L.X. Zhou, H.J. Wang, J.W. Elkins and B. Hall

2012-38
12: 10033-10050

Abstract/Summary: 

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.

© 2012 the authors