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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 11, issue 2 | Copyright
Atmos. Chem. Phys., 11, 465-477, 2011
https://doi.org/10.5194/acp-11-465-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 17 Jan 2011

Research article | 17 Jan 2011

Californian forest fire plumes over Southwestern British Columbia: lidar, sunphotometry, and mountaintop chemistry observations

I. McKendry1, K. Strawbridge2, M. L. Karumudi3, N. O'Neill3, A. M. Macdonald4, R. Leaitch4, D. Jaffe5, P. Cottle1, S. Sharma4, P. Sheridan6, and J. Ogren6 I. McKendry et al.
  • 1Department of Geography, the University of British Columbia, Vancouver, British Columbia, Canada
  • 2Science and Technology Branch, Environment Canada, Centre for Atmospheric Research Experiments, Egbert, Ontario, Canada
  • 3Université de Sherbrooke, Sherbrooke, QC, Canada
  • 4Science and Technology Branch, Environment Canada, 4905 Dufferin Street, Toronto, Ontario M3H 5T4, Canada
  • 5Atmospheric and Environmental Chemistry, University of Washington-Bothell, Seattle, USA
  • 6NOAA-Earth System Research Laboratory, Global Monitoring Division, Boulder, Colorado, USA

Abstract. Forest fires in Northern California and Oregon were responsible for two significant regional scale aerosol transport events observed in southern British Columbia during summer 2008. A combination of ground based (CORALNet) and satellite (CALIPSO) lidar, sunphotometry and high altitude chemistry observations permitted unprecedented characterization of forest fire plume height and mixing as well as description of optical properties and physicochemistry of the aerosol. In southwestern BC, lidar observations show the smoke to be mixed through a layer extending to 5–6 km a.g.l. where the aerosol was confined by an elevated inversion in both cases. Depolarization ratios for a trans-Pacific dust event (providing a basis for comparison) and the two smoke events were consistent with observations of dust and smoke events elsewhere and permit discrimination of aerosol events in the region. Based on sunphotometry, the Aerosol Optical Thicknesses (AOT) reached maxima of ~0.7 and ~0.4 for the two events respectively. Dubovik-retrieval values of reff, f during both the June/July and August events varied between about 0.13 and 0.15 μm and confirm the dominance of accumulation mode size particles in the forest fire plumes. Both Whistler Peak and Mount Bachelor Observatory data show that smoke events are accompanied by elevated CO and O3 concentrations as well as elevated K+/SO4 ratios. In addition to documenting the meteorology and physic-chemical characteristics of two regional scale biomass burning plumes, this study demonstrates the positive analytical synergies arising from the suite of measurements now in place in the Pacific Northwest, and complemented by satellite borne instruments.

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