journal article Dec 01, 2006

CTM study of changes in tropospheric hydroxyl distribution 1990–2001 and its impact on methane

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Abstract
Impacts of emission changes on hydroxyl (OH) and methane lifetime in the troposphere are studied using an emission inventory for the period 1990–2001 as input to a global Chemical Transport Model (CTM) run with repeated year 2000 meteorology. Global OH is estimated to increase, in average by 0.08% per year, with exception of 1997 and 1998 when deviations from the trend result from unusually large biomass burning emissions. The global OH evolution is highly dependent on the CO to NOx emission ratio, and a statistically significant linear relation between this ratio and the OH concentration is found. However, we find large regional variations of OH distributions and methane loss. One third of a calculated increase in global average methane loss (0.50% per year) can be explained by OH changes resulting from emission changes of CO, NOx and NMVOCs, while two third is due to increases in methane itself.
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References
29
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Dalsøren S. B.(2001) 3D CTM studies of biomass burning and changes in atmospheric oxidation capacity scientiarum thesis 185 pp. Dep. of Geophys. Univ. of Oslo Oslo.
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Cited By
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Role of atmospheric oxidation in recent methane growth

Matthew Rigby, Stephen A. Montzka · 2017

Proceedings of the National Academy...
Atmospheric Chemistry and Physics
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46
Citations
29
References
Details
Published
Dec 01, 2006
Vol/Issue
33(23)
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Cite This Article
Stig B. Dalsøren, Ivar S. A. Isaksen (2006). CTM study of changes in tropospheric hydroxyl distribution 1990–2001 and its impact on methane. Geophysical Research Letters, 33(23). https://doi.org/10.1029/2006gl027295
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