Overview: Oxidant and particle photochemical processes above a south-east Asian tropical rain forest (the OP3 project): introduction, rationale, location characteristics and tools
Hewitt, C. N.; Lee, J.; Barkley, M. P.; Carslaw, N.; Chappell, N. A.; Coe, H.; Collier, C.; Commane, R.; Davies, F.; Di Carlo, P.; Di Marco, C.; Edwards, P. M.; Evans, M.J.; Fowler, D.; Furneaux, K. L.; Gallagher, M.; Guenther, A.; Heard, D. E.; Helfter, C.; Hopkins, J.; Ingham, T.; Irwin, M.; Jones, C.; Karunaharan, A.; Langford, B.; Lewis, A.; Lim, S. F.; MacDonald, S. M.; MacKenzie, A. R.; Mahajan, A. S.; Malpass, S.; McFiggans, G.; Mills, G.; Misztal, P.; Moller, S.; Monks, P. S.; Nemitz, E.; Nicolas-Perea, V.; Oetjen, H.; Oram, D.; Palmer, P. I.; Phillips, G.; Plane, J. M. C.; Pugh, T.; Pyle, J. A.; Reeves, C. E.; Robinson, N. H.; Stewart, D.; Stone, D.; Whalley, L. K.; Yin, X.. 2010 Overview: Oxidant and particle photochemical processes above a south-east Asian tropical rain forest (the OP3 project): introduction, rationale, location characteristics and tools. Atmospheric Chemistry and Physics, 10. 169-199. 10.5194/acp-10-169-2010Full text not available from this repository.
In April–July 2008, intensive measurements were made of atmospheric composition and chemistry in Sabah, Malaysia, as part of the “Oxidant and particle photochemical processes above a South-East Asian tropical rainforest” (OP3) project. Fluxes and concentrations of trace gases and particles were made from and above the rainforest canopy at the Bukit Atur Global Atmosphere Watch station and at the nearby Sabahmas oil palm plantation, using both ground-based and airborne measurements. Here, the measurement and modelling strategies used, the characteristics of the sites and an overview of data obtained are described. Composition measurements show that the rainforest site was not significantly impacted by anthropogenic pollution, and this is confirmed by satellite retrievals of NO2 and HCHO. The dominant modulators of atmospheric chemistry at the rainforest site were therefore emissions of BVOCs and soil emissions of reactive nitrogen oxides. At the observed BVOC:NOx volume mixing ratio (100 pptv/pptv), current chemical models suggest that daytime maximum OH concentrations should be ca. 105 radicals cm−3, but observed OH concentrations were an order of magnitude greater than this. We confirm, therefore, previous measurements that suggest that an unexplained source of OH must exist above tropical rainforest and we continue to interrogate the data to find explanations for this.
|Item Type:||Publication - Article|
|Digital Object Identifier (DOI):||10.5194/acp-10-169-2010|
|Programmes:||CEH Topics & Objectives 2009 - 2012 > Biogeochemistry > BGC Topic 2 - Biogeochemistry and Climate System Processes > BGC - 2.1 - Quantify & model processes that control the emission, fate and bioavailability of pollutants|
|CEH Sections:||Billett (to November 2013)|
|Additional Information. Not used in RCUK Gateway to Research.:||Full text available from Official URL: http://www.atmos-chem-phys.net/10/169/2010/acp-10-169-2010.pdf. PLEASE NOTE: There is a corrigenda to this paper in Atmospheric Chemistry and Physics, 10, 563-563.|
|NORA Subject Terms:||Atmospheric Sciences|
|Date made live:||24 Feb 2010 15:41|
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