1Department of Chemistry, University of Wisconsin-Madison, Madison, Wisconsin, USA
2Department of Land, Air, and Water Resources, Univ. of California-Davis, Davis, California, USA
3NOAA Earth System Research Laboratory and Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, USA
4Department of Environmental Science, Policy, and Management, University of California, Berkeley, California, USA
5Department of Chemistry, University of California, Berkeley, California, USA
6Department of Chemistry, University of Washington, Seattle, Washington, USA
7CIRES and Department of Chemistry and Biochemistry, University of Colorado, Boulder, Colorado, USA
8Department of Meteorology, Pennsylvania State University, University Park, Pennsylvania, USA
anow at: Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
bnow at: Air Force Office of Scientific Research-Physics and Electronics Directorate, Arlington, Virginia, USA
cnow at: Chemistry Department, Reed College, Portland, Oregon, USA
dnow at: Air Force Space and Missile Systems Center Weather Directorate, Los Angeles, California, USA
enow at: Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, Los Angeles, California, USA
fnow at: Chemistry & Biochemistry Department, Loyola Marymount University, Los Angeles, California, USA
gnow at: Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, California, USA
hnow at: Department of Chemistry, University of Wisconsin-Madison, Madison, Wisconsin, USA
inow at: Alion Science and Technology and EPA Office of Research and Development, Research Triangle Park, North Carolina, USA
jnow at: Department of Chemistry, Colorado State University, Fort Collins, Colorado, USA
know at: Program in Atmospheric and Oceanic Sciences, Princeton University, Princeton, New Jersey, USA
Received: 29 Mar 2011 – Published in Atmos. Chem. Phys. Discuss.: 05 May 2011
Abstract. We present roughly one month of high time-resolution, direct, in situ measurements of gas-phase glyoxal acquired during the BEARPEX 2007 field campaign. The research site, located on a ponderosa pine plantation in the Sierra Nevada mountains, is strongly influenced by biogenic volatile organic compounds (BVOCs); thus this data adds to the few existing measurements of glyoxal in BVOC-dominated areas. The short lifetime of glyoxal of ~1 h, the fact that glyoxal mixing ratios are much higher during high temperature periods, and the results of a photochemical model demonstrate that glyoxal is strongly influenced by BVOC precursors during high temperature periods.
Revised: 15 Aug 2011 – Accepted: 22 Aug 2011 – Published: 01 Sep 2011
A zero-dimensional box model using near-explicit chemistry from the Leeds Master Chemical Mechanism v3.1 was used to investigate the processes controlling glyoxal chemistry during BEARPEX 2007. The model showed that MBO is the most important glyoxal precursor (~67 %), followed by isoprene (~26 %) and methylchavicol (~6 %), a precursor previously not commonly considered for glyoxal production. The model calculated a noon lifetime for glyoxal of ~0.9 h, making glyoxal well suited as a local tracer of VOC oxidation in a forested rural environment; however, the modeled glyoxal mixing ratios over-predicted measured glyoxal by a factor 2 to 5. Loss of glyoxal to aerosol was not found to be significant, likely as a result of the very dry conditions, and could not explain the over-prediction. Although several parameters, such as an approximation for advection, were found to improve the model measurement discrepancy, reduction in OH was by far the most effective. Reducing model OH concentrations to half the measured values decreased the glyoxal over-prediction from a factor of 2.4 to 1.1, as well as the overprediction of HO2 from a factor of 1.64 to 1.14. Our analysis has shown that glyoxal is particularly sensitive to OH concentration compared to other BVOC oxidation products. This relationship arises from (i) the predominantly secondary- or higher-generation production of glyoxal from (mainly OH-driven, rather than O3-driven) BVOC oxidation at this site and (ii) the relative importance of photolysis in glyoxal loss as compared to reaction with OH. We propose that glyoxal is a useful tracer for OH-driven BVOC oxidation chemistry.
Huisman, A. J., Hottle, J. R., Galloway, M. M., DiGangi, J. P., Coens, K. L., Choi, W., Faloona, I. C., Gilman, J. B., Kuster, W. C., de Gouw, J., Bouvier-Brown, N. C., Goldstein, A. H., LaFranchi, B. W., Cohen, R. C., Wolfe, G. M., Thornton, J. A., Docherty, K. S., Farmer, D. K., Cubison, M. J., Jimenez, J. L., Mao, J., Brune, W. H., and Keutsch, F. N.: Photochemical modeling of glyoxal at a rural site: observations and analysis from BEARPEX 2007, Atmos. Chem. Phys., 11, 8883-8897, doi:10.5194/acp-11-8883-2011, 2011.