Improving measurements of SF<sub>6</sub> for the study of atmospheric transport and emissions

Sulfur hexafluoride (SF<sub>6</sub>) is a potent greenhouse gas and useful atmospheric tracer. Measurements of SF<sub>6</sub> on global and regional scales are necessary to estimate emissions and to verify or examine the performance of atmospheric transport models. Typical pr...

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Main Authors: D. F. Hurst, F. L. Moore, J. H. Butler, M. Rigby, J. D. Nance, D. J. Mondeel, G. S. Dutton, B. D. Hall, J. W. Elkins
Format: Article
Language:English
Published: Copernicus Publications 2011-11-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/4/2441/2011/amt-4-2441-2011.pdf
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spelling doaj-e091b7ff538d48058af26fa42cd849ea2020-11-24T23:18:09ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482011-11-014112441245110.5194/amt-4-2441-2011Improving measurements of SF<sub>6</sub> for the study of atmospheric transport and emissionsD. F. HurstF. L. MooreJ. H. ButlerM. RigbyJ. D. NanceD. J. MondeelG. S. DuttonB. D. HallJ. W. ElkinsSulfur hexafluoride (SF<sub>6</sub>) is a potent greenhouse gas and useful atmospheric tracer. Measurements of SF<sub>6</sub> on global and regional scales are necessary to estimate emissions and to verify or examine the performance of atmospheric transport models. Typical precision for common gas chromatographic methods with electron capture detection (GC-ECD) is 1–2%. We have modified a common GC-ECD method to achieve measurement precision of 0.5% or better. Global mean SF<sub>6</sub> measurements were used to examine changes in the growth rate of SF<sub>6</sub> and corresponding SF<sub>6</sub> emissions. Global emissions and mixing ratios from 2000–2008 are consistent with recently published work. More recent observations show a 10% decline in SF<sub>6</sub> emissions in 2008–2009, which seems to coincide with a decrease in world economic output. This decline was short-lived, as the global SF<sub>6</sub> growth rate has recently increased to near its 2007–2008 maximum value of 0.30&plusmn;0.03 pmol mol<sup>−1</sup> (ppt) yr<sup>−1</sup> (95% C.L.).http://www.atmos-meas-tech.net/4/2441/2011/amt-4-2441-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. F. Hurst
F. L. Moore
J. H. Butler
M. Rigby
J. D. Nance
D. J. Mondeel
G. S. Dutton
B. D. Hall
J. W. Elkins
spellingShingle D. F. Hurst
F. L. Moore
J. H. Butler
M. Rigby
J. D. Nance
D. J. Mondeel
G. S. Dutton
B. D. Hall
J. W. Elkins
Improving measurements of SF<sub>6</sub> for the study of atmospheric transport and emissions
Atmospheric Measurement Techniques
author_facet D. F. Hurst
F. L. Moore
J. H. Butler
M. Rigby
J. D. Nance
D. J. Mondeel
G. S. Dutton
B. D. Hall
J. W. Elkins
author_sort D. F. Hurst
title Improving measurements of SF<sub>6</sub> for the study of atmospheric transport and emissions
title_short Improving measurements of SF<sub>6</sub> for the study of atmospheric transport and emissions
title_full Improving measurements of SF<sub>6</sub> for the study of atmospheric transport and emissions
title_fullStr Improving measurements of SF<sub>6</sub> for the study of atmospheric transport and emissions
title_full_unstemmed Improving measurements of SF<sub>6</sub> for the study of atmospheric transport and emissions
title_sort improving measurements of sf<sub>6</sub> for the study of atmospheric transport and emissions
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2011-11-01
description Sulfur hexafluoride (SF<sub>6</sub>) is a potent greenhouse gas and useful atmospheric tracer. Measurements of SF<sub>6</sub> on global and regional scales are necessary to estimate emissions and to verify or examine the performance of atmospheric transport models. Typical precision for common gas chromatographic methods with electron capture detection (GC-ECD) is 1–2%. We have modified a common GC-ECD method to achieve measurement precision of 0.5% or better. Global mean SF<sub>6</sub> measurements were used to examine changes in the growth rate of SF<sub>6</sub> and corresponding SF<sub>6</sub> emissions. Global emissions and mixing ratios from 2000–2008 are consistent with recently published work. More recent observations show a 10% decline in SF<sub>6</sub> emissions in 2008–2009, which seems to coincide with a decrease in world economic output. This decline was short-lived, as the global SF<sub>6</sub> growth rate has recently increased to near its 2007–2008 maximum value of 0.30&plusmn;0.03 pmol mol<sup>−1</sup> (ppt) yr<sup>−1</sup> (95% C.L.).
url http://www.atmos-meas-tech.net/4/2441/2011/amt-4-2441-2011.pdf
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