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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.
Mühle, J.
Weiss, R. F.
Salameh, P. K.
Kim, J.
Li, S.
Park, S.
Kim, K.-R.
Young, D.
O'Doherty, S.
Source :
Atmospheric Chemistry & Physics; 2012, Vol. 12 Issue 21, p10033-10050, 25p
Publication Year :
2012

Abstract

HCFC-22 (CHClF<subscript>2</subscript>, 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 halo-carbons 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. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
16807316
Volume :
12
Issue :
21
Database :
Complementary Index
Journal :
Atmospheric Chemistry & Physics
Publication Type :
Academic Journal
Accession number :
83916118
Full Text :
https://doi.org/10.5194/acp-12-10033-2012