© Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics

Abstract. Aerosol measurements at Barrow, Alaska dur-ing the past 30 years have identified the long range trans-port of pollution associated with Arctic Haze as well as ocean-derived aerosols of more local origin. Here, we fo-cus on measurements of aerosol chemical composition to as-sess (1) trends...

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Main Authors: P. K. Quinn, T. S. Bates, K. Schulz, G. E. Shaw
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2009
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.615.1039
http://www.atmos-chem-phys.org/9/8883/2009/acp-9-8883-2009.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.615.1039 2023-05-15T14:52:02+02:00 © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics P. K. Quinn T. S. Bates K. Schulz G. E. Shaw The Pennsylvania State University CiteSeerX Archives 2009 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.615.1039 http://www.atmos-chem-phys.org/9/8883/2009/acp-9-8883-2009.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.615.1039 http://www.atmos-chem-phys.org/9/8883/2009/acp-9-8883-2009.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.atmos-chem-phys.org/9/8883/2009/acp-9-8883-2009.pdf text 2009 ftciteseerx 2016-01-08T14:42:12Z Abstract. Aerosol measurements at Barrow, Alaska dur-ing the past 30 years have identified the long range trans-port of pollution associated with Arctic Haze as well as ocean-derived aerosols of more local origin. Here, we fo-cus on measurements of aerosol chemical composition to as-sess (1) trends in Arctic Haze aerosol and implications for source regions, (2) the interaction between pollution-derived and ocean-derived aerosols and the resulting impacts on the chemistry of the Arctic boundary layer, and (3) the response of aerosols to a changing climate. Aerosol chemical compo-sition measured at Barrow, AK during the Arctic haze season is compared for the years 1976–1977 and 1997–2008. Based on these two data sets, concentrations of non-sea salt (nss) sulfate (SO=4) and non-crustal (nc) vanadium (V) have de-creased by about 60 % over this 30 year period. Consistency in the ratios of nss SO=4 /ncV and nc manganese (Mn)/ncV between the two data sets indicates that, although emissions have decreased in the source regions, the source regions have remained the same over this time period. The measurements from 1997–2008 indicate that, during the haze season, the nss SO=4 aerosol at Barrow is becoming less neutralized by ammonium (NH+4) yielding an increasing sea salt aerosol chloride (Cl−) deficit. The expected consequence is an in-crease in the release of Cl atoms to the atmosphere and a change in the lifetime of volatile organic compounds (VOCs) including methane. In addition, summertime concentra-tions of biogenically-derived methanesulfonate (MSA−) and Correspondence to: P. K. Quinn Text Arctic Barrow Alaska Unknown Arctic
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description Abstract. Aerosol measurements at Barrow, Alaska dur-ing the past 30 years have identified the long range trans-port of pollution associated with Arctic Haze as well as ocean-derived aerosols of more local origin. Here, we fo-cus on measurements of aerosol chemical composition to as-sess (1) trends in Arctic Haze aerosol and implications for source regions, (2) the interaction between pollution-derived and ocean-derived aerosols and the resulting impacts on the chemistry of the Arctic boundary layer, and (3) the response of aerosols to a changing climate. Aerosol chemical compo-sition measured at Barrow, AK during the Arctic haze season is compared for the years 1976–1977 and 1997–2008. Based on these two data sets, concentrations of non-sea salt (nss) sulfate (SO=4) and non-crustal (nc) vanadium (V) have de-creased by about 60 % over this 30 year period. Consistency in the ratios of nss SO=4 /ncV and nc manganese (Mn)/ncV between the two data sets indicates that, although emissions have decreased in the source regions, the source regions have remained the same over this time period. The measurements from 1997–2008 indicate that, during the haze season, the nss SO=4 aerosol at Barrow is becoming less neutralized by ammonium (NH+4) yielding an increasing sea salt aerosol chloride (Cl−) deficit. The expected consequence is an in-crease in the release of Cl atoms to the atmosphere and a change in the lifetime of volatile organic compounds (VOCs) including methane. In addition, summertime concentra-tions of biogenically-derived methanesulfonate (MSA−) and Correspondence to: P. K. Quinn
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author P. K. Quinn
T. S. Bates
K. Schulz
G. E. Shaw
spellingShingle P. K. Quinn
T. S. Bates
K. Schulz
G. E. Shaw
© Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics
author_facet P. K. Quinn
T. S. Bates
K. Schulz
G. E. Shaw
author_sort P. K. Quinn
title © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics
title_short © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics
title_full © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics
title_fullStr © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics
title_full_unstemmed © Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics
title_sort © author(s) 2009. this work is distributed under the creative commons attribution 3.0 license. atmospheric chemistry and physics
publishDate 2009
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.615.1039
http://www.atmos-chem-phys.org/9/8883/2009/acp-9-8883-2009.pdf
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http://www.atmos-chem-phys.org/9/8883/2009/acp-9-8883-2009.pdf
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