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Global and regional emission estimates for HCFC-22

Authors :
Saikawa, E.
Rigby, M.
Prinn, R.G.
Montzka, S.A.
Miller, B.R.
Kuijpers, L.J.M.
Fraser, P.J.B.
Vollmer, M.K.
Saito, T.
Yokouchi, Y.
Harth, C.M.
Muhle, J.
Weiss, R.F.
Salameh, P.K.
Kim, J.
Li, S.
Park, S.
Kim, K.R.
Young, D.
O'Doherty, S.
Simmonds, P.G.
McCulloch, A.
Krummel, P.B.
Steele, L.P.
Lunder, C.
Hermansen, O.
Maione, M.
Arduini, J.
Yao, B.
Zhou, L.X.
Wang, H.J.
Elkins, J.W.
Hall, B.
Saikawa, E.
Rigby, M.
Prinn, R.G.
Montzka, S.A.
Miller, B.R.
Kuijpers, L.J.M.
Fraser, P.J.B.
Vollmer, M.K.
Saito, T.
Yokouchi, Y.
Harth, C.M.
Muhle, J.
Weiss, R.F.
Salameh, P.K.
Kim, J.
Li, S.
Park, S.
Kim, K.R.
Young, D.
O'Doherty, S.
Simmonds, P.G.
McCulloch, A.
Krummel, P.B.
Steele, L.P.
Lunder, C.
Hermansen, O.
Maione, M.
Arduini, J.
Yao, B.
Zhou, L.X.
Wang, H.J.
Elkins, J.W.
Hall, B.
Source :
Atmospheric Chemistry and Physics vol.12 (2012) nr.21 p.10033-10050 [ISSN 1680-7316]
Publication Year :
2012

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

Details

Database :
OAIster
Journal :
Atmospheric Chemistry and Physics vol.12 (2012) nr.21 p.10033-10050 [ISSN 1680-7316]
Notes :
Saikawa, E.
Publication Type :
Electronic Resource
Accession number :
edsoai.on1359163898
Document Type :
Electronic Resource