Sources of light-absorbing aerosol in arctic snow and their seasonal variation

Two data sets consisting of measurements of light absorbing aerosols (LAA) in arctic snow together with suites of other corresponding chemical constituents are presented; the first from Siberia, Greenland and near the North Pole obtained in 2008, and the second from the Canadian arctic obtained in 2...

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Main Authors: Dean A. Hegg, Stephen G. Warren, Thomas C. Grenfell, Sarah J Doherty, Antony D. Clarke
Format: Article
Language:English
Published: Copernicus Publications 2010-11-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/10/10923/2010/acp-10-10923-2010.pdf
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spelling doaj-45bfff2208964c66b67fc2a42c14054c2020-11-24T22:11:23ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242010-11-011022109231093810.5194/acp-10-10923-2010Sources of light-absorbing aerosol in arctic snow and their seasonal variationDean A. HeggStephen G. WarrenThomas C. GrenfellSarah J DohertyAntony D. ClarkeTwo data sets consisting of measurements of light absorbing aerosols (LAA) in arctic snow together with suites of other corresponding chemical constituents are presented; the first from Siberia, Greenland and near the North Pole obtained in 2008, and the second from the Canadian arctic obtained in 2009. A preliminary differentiation of the LAA into black carbon (BC) and non-BC LAA is done. Source attribution of the light absorbing aerosols was done using a positive matrix factorization (PMF) model. Four sources were found for each data set (crop and grass burning, boreal biomass burning, pollution and marine). For both data sets, the crops and grass biomass burning was the main source of both LAA species, suggesting the non-BC LAA was brown carbon. Depth profiles at most of the sites allowed assessment of the seasonal variation in the source strengths. The biomass burning sources dominated in the spring but pollution played a more significant (though rarely dominant) role in the fall, winter and, for Greenland, summer. The PMF analysis is consistent with trajectory analysis and satellite fire maps. http://www.atmos-chem-phys.net/10/10923/2010/acp-10-10923-2010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Dean A. Hegg
Stephen G. Warren
Thomas C. Grenfell
Sarah J Doherty
Antony D. Clarke
spellingShingle Dean A. Hegg
Stephen G. Warren
Thomas C. Grenfell
Sarah J Doherty
Antony D. Clarke
Sources of light-absorbing aerosol in arctic snow and their seasonal variation
Atmospheric Chemistry and Physics
author_facet Dean A. Hegg
Stephen G. Warren
Thomas C. Grenfell
Sarah J Doherty
Antony D. Clarke
author_sort Dean A. Hegg
title Sources of light-absorbing aerosol in arctic snow and their seasonal variation
title_short Sources of light-absorbing aerosol in arctic snow and their seasonal variation
title_full Sources of light-absorbing aerosol in arctic snow and their seasonal variation
title_fullStr Sources of light-absorbing aerosol in arctic snow and their seasonal variation
title_full_unstemmed Sources of light-absorbing aerosol in arctic snow and their seasonal variation
title_sort sources of light-absorbing aerosol in arctic snow and their seasonal variation
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2010-11-01
description Two data sets consisting of measurements of light absorbing aerosols (LAA) in arctic snow together with suites of other corresponding chemical constituents are presented; the first from Siberia, Greenland and near the North Pole obtained in 2008, and the second from the Canadian arctic obtained in 2009. A preliminary differentiation of the LAA into black carbon (BC) and non-BC LAA is done. Source attribution of the light absorbing aerosols was done using a positive matrix factorization (PMF) model. Four sources were found for each data set (crop and grass burning, boreal biomass burning, pollution and marine). For both data sets, the crops and grass biomass burning was the main source of both LAA species, suggesting the non-BC LAA was brown carbon. Depth profiles at most of the sites allowed assessment of the seasonal variation in the source strengths. The biomass burning sources dominated in the spring but pollution played a more significant (though rarely dominant) role in the fall, winter and, for Greenland, summer. The PMF analysis is consistent with trajectory analysis and satellite fire maps.
url http://www.atmos-chem-phys.net/10/10923/2010/acp-10-10923-2010.pdf
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