Isoprene oxidation mechanisms: measurements and modelling of OH and HO<sub>2</sub> over a South-East Asian tropical rainforest during the OP3 field campaign

Forests are the dominant source of volatile organic compounds into the atmosphere, with isoprene being the most significant species. The oxidation chemistry of these compounds is a significant driver of local, regional and global atmospheric composition. Observations made over Borneo during the OP3...

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Main Authors: C. E. Reeves, D. Oram, P. S. Monks, A. C. Lewis, R. J. Leigh, J. Hopkins, D. M. Brookes, A. R. Rickard, T. Ingham, R. Commane, M. J. Evans, P. M. Edwards, D. Stone, D. Stewart, D. E. Heard
Format: Article
Language:English
Published: Copernicus Publications 2011-07-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/11/6749/2011/acp-11-6749-2011.pdf
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author C. E. Reeves
D. Oram
P. S. Monks
A. C. Lewis
R. J. Leigh
J. Hopkins
D. M. Brookes
A. R. Rickard
T. Ingham
R. Commane
M. J. Evans
P. M. Edwards
D. Stone
D. Stewart
D. E. Heard
author_facet C. E. Reeves
D. Oram
P. S. Monks
A. C. Lewis
R. J. Leigh
J. Hopkins
D. M. Brookes
A. R. Rickard
T. Ingham
R. Commane
M. J. Evans
P. M. Edwards
D. Stone
D. Stewart
D. E. Heard
author_sort C. E. Reeves
collection DOAJ
description Forests are the dominant source of volatile organic compounds into the atmosphere, with isoprene being the most significant species. The oxidation chemistry of these compounds is a significant driver of local, regional and global atmospheric composition. Observations made over Borneo during the OP3 project in 2008, together with an observationally constrained box model are used to assess our understanding of this oxidation chemistry. In line with previous work in tropical forests, we find that the standard model based on MCM chemistry significantly underestimates the observed OH concentrations. Geometric mean observed to modelled ratios of OH and HO<sub>2</sub> in airmasses impacted with isoprene are 5.32<sub>&minus;4.43</sub><sup>+3.68</sup> and 1.18<sub>&minus;0.30</sub><sup>+0.30</sup> respectively, with 68 % of the observations being within the specified variation. We implement a variety of mechanistic changes into the model, including epoxide formation and unimolecular decomposition of isoprene peroxy radicals, and assess their impact on the model success. We conclude that none of the current suggestions can simultaneously remove the bias from both OH and HO<sub>2</sub> simulations and believe that detailed laboratory studies are now needed to resolve this issue.
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spelling doaj.art-a5d1f1be811b42edafa9293c683fa3c22022-12-22T03:23:18ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242011-07-0111136749677110.5194/acp-11-6749-2011Isoprene oxidation mechanisms: measurements and modelling of OH and HO<sub>2</sub> over a South-East Asian tropical rainforest during the OP3 field campaignC. E. ReevesD. OramP. S. MonksA. C. LewisR. J. LeighJ. HopkinsD. M. BrookesA. R. RickardT. InghamR. CommaneM. J. EvansP. M. EdwardsD. StoneD. StewartD. E. HeardForests are the dominant source of volatile organic compounds into the atmosphere, with isoprene being the most significant species. The oxidation chemistry of these compounds is a significant driver of local, regional and global atmospheric composition. Observations made over Borneo during the OP3 project in 2008, together with an observationally constrained box model are used to assess our understanding of this oxidation chemistry. In line with previous work in tropical forests, we find that the standard model based on MCM chemistry significantly underestimates the observed OH concentrations. Geometric mean observed to modelled ratios of OH and HO<sub>2</sub> in airmasses impacted with isoprene are 5.32<sub>&minus;4.43</sub><sup>+3.68</sup> and 1.18<sub>&minus;0.30</sub><sup>+0.30</sup> respectively, with 68 % of the observations being within the specified variation. We implement a variety of mechanistic changes into the model, including epoxide formation and unimolecular decomposition of isoprene peroxy radicals, and assess their impact on the model success. We conclude that none of the current suggestions can simultaneously remove the bias from both OH and HO<sub>2</sub> simulations and believe that detailed laboratory studies are now needed to resolve this issue.http://www.atmos-chem-phys.net/11/6749/2011/acp-11-6749-2011.pdf
spellingShingle C. E. Reeves
D. Oram
P. S. Monks
A. C. Lewis
R. J. Leigh
J. Hopkins
D. M. Brookes
A. R. Rickard
T. Ingham
R. Commane
M. J. Evans
P. M. Edwards
D. Stone
D. Stewart
D. E. Heard
Isoprene oxidation mechanisms: measurements and modelling of OH and HO<sub>2</sub> over a South-East Asian tropical rainforest during the OP3 field campaign
Atmospheric Chemistry and Physics
title Isoprene oxidation mechanisms: measurements and modelling of OH and HO<sub>2</sub> over a South-East Asian tropical rainforest during the OP3 field campaign
title_full Isoprene oxidation mechanisms: measurements and modelling of OH and HO<sub>2</sub> over a South-East Asian tropical rainforest during the OP3 field campaign
title_fullStr Isoprene oxidation mechanisms: measurements and modelling of OH and HO<sub>2</sub> over a South-East Asian tropical rainforest during the OP3 field campaign
title_full_unstemmed Isoprene oxidation mechanisms: measurements and modelling of OH and HO<sub>2</sub> over a South-East Asian tropical rainforest during the OP3 field campaign
title_short Isoprene oxidation mechanisms: measurements and modelling of OH and HO<sub>2</sub> over a South-East Asian tropical rainforest during the OP3 field campaign
title_sort isoprene oxidation mechanisms measurements and modelling of oh and ho sub 2 sub over a south east asian tropical rainforest during the op3 field campaign
url http://www.atmos-chem-phys.net/11/6749/2011/acp-11-6749-2011.pdf
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