Levoglucosan levels at background sites in Europe for assessing the impact of biomass combustion on the European aerosol background

Atmospheric levoglucosan has been determined as a proxy for “biomass smoke” in samples from six background stations on a west–east transect extending from the Atlantic (Azores) to the mid‐European background site KPZ (K‐Puszta, Hungary). Concentration levels of levoglucosan (biannual averages) in th...

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Published in:Journal of Geophysical Research - Atmospheres Vol. 112; no. D23; pp. D23S05 - n/a
Main Authors: Puxbaum, Hans, Caseiro, Alexandre, Sánchez-Ochoa, Asunción, Kasper-Giebl, Anne, Claeys, Magda, Gelencsér, András, Legrand, Michel, Preunkert, Susanne, Pio, Casimiro
Format: Journal Article
Language:English
Published: American Geophysical Union 16-12-2007
Blackwell Publishing Ltd
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Summary:Atmospheric levoglucosan has been determined as a proxy for “biomass smoke” in samples from six background stations on a west–east transect extending from the Atlantic (Azores) to the mid‐European background site KPZ (K‐Puszta, Hungary). Concentration levels of levoglucosan (biannual averages) in the west–east transect range from 0.005 μg/m3 at the oceanic background site AZO (Azores) to 0.52 μg/m3 at AVE (Aveiro, Portugal). The atmospheric concentration of “biomass smoke” (biannual averages) was derived from the levoglucosan data with wood‐type‐specific conversion factors. Annual averages of wood smoke levels ranged from 0.05 μg/m3 at AZO to 4.3 μg/m3 at AVE. Winter (DJF) averages at the low‐level sites AVE and KPZ were 10.8 and 6.7 μg/m3, respectively. Relative contributions of biomass smoke to organic matter (OM) range from around 9–11% at the elevated sites SIL, PDD and SBO, as well as for AZO, to 36% at the low‐level site AVE and 28% at KPZ. Surprisingly high relative concentrations of biomass smoke in OM (68 and 47%) were observed for wintry conditions at the continental low‐level CARBOSOL sites AVE and KPZ. Thus biomass smoke is a very important constituent of the organic material in the mid and west European background with summer contributions to organic matter of around 1–6% and winter levels of around 20% at the elevated mountain sites and 47–68% at rural flat terrain sites, not including secondary organic aerosol from biomass combustion sources.
Bibliography:istex:0906A1891F0EE62CB590065011A3A9AA98F8B783
ark:/67375/WNG-Z5ZF1LBT-W
ArticleID:2006JD008114
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0148-0227
2169-897X
2156-2202
2169-8996
DOI:10.1029/2006JD008114