Scattering coefficient, size distribution and the transport process of tropospheric aerosol in the Arctic region observed with an aircraft during ASTAR 2000/2004 and AAMP 2002 campaign in spring
Airborne aerosol measurements of the Arctic haze were carried out during three campaigns, Arctic Study of Tropospheric Aerosol and Radiation 2000 (ASTAR 2000), the Arctic Airborne Measurement Program 2002 (AAMP 2002) and ASTAR 2004. Aircraft used for the campaigns were Dornier for ASTAR 2000 2004 an...
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National Institute of Polar Research
2010
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fttriple:oai:gotriple.eu:oai:doaj.org/article:30cb2dfd6cdb4627b0f002511292e54e 2023-05-15T14:32:51+02:00 Scattering coefficient, size distribution and the transport process of tropospheric aerosol in the Arctic region observed with an aircraft during ASTAR 2000/2004 and AAMP 2002 campaign in spring Sadamu Yamagata Keiichiro Hara Atsushi Matsuki 2010-12-01 https://doi.org/10.15094/00009590 https://doaj.org/article/30cb2dfd6cdb4627b0f002511292e54e en other eng National Institute of Polar Research doi:10.15094/00009590 0085-7289 2432-079X https://doaj.org/article/30cb2dfd6cdb4627b0f002511292e54e undefined Antarctic Record, Vol 54, Iss special issue, Pp 868-881 (2010) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2010 fttriple https://doi.org/10.15094/00009590 2023-01-22T19:23:19Z Airborne aerosol measurements of the Arctic haze were carried out during three campaigns, Arctic Study of Tropospheric Aerosol and Radiation 2000 (ASTAR 2000), the Arctic Airborne Measurement Program 2002 (AAMP 2002) and ASTAR 2004. Aircraft used for the campaigns were Dornier for ASTAR 2000 2004 and Gulfstream II for AAMP 2002. For all measurements aerosol particles were introduced into the cabin through stainless inlets and distributed to several instruments via a diffuser. Scattering coefficient of aerosol particles measured with an integrating nephelometer during the Arctic haze period showed a distinct difference between the lower, i.e. up to around 4000 m, and higher troposphere. Meanwhile, scattering coefficients in higher troposphere during the Arctic haze were in the same degree with those after the Arctic haze. Size distribution obtained from the data of a particle counter indicates that aerosol particles in accumulation mode during the Arctic haze have larger geometric mean diameter than those after the haze season, which reflects the aged air mass in the Arctic haze. "Curtain flight" which was carried out to reveal the fine structure of the haze layer showed that aerosol particles are transported in the isentropic plane. Article in Journal/Newspaper Arctic Unknown Arctic |
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language |
English |
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geo envir Sadamu Yamagata Keiichiro Hara Atsushi Matsuki Scattering coefficient, size distribution and the transport process of tropospheric aerosol in the Arctic region observed with an aircraft during ASTAR 2000/2004 and AAMP 2002 campaign in spring |
topic_facet |
geo envir |
description |
Airborne aerosol measurements of the Arctic haze were carried out during three campaigns, Arctic Study of Tropospheric Aerosol and Radiation 2000 (ASTAR 2000), the Arctic Airborne Measurement Program 2002 (AAMP 2002) and ASTAR 2004. Aircraft used for the campaigns were Dornier for ASTAR 2000 2004 and Gulfstream II for AAMP 2002. For all measurements aerosol particles were introduced into the cabin through stainless inlets and distributed to several instruments via a diffuser. Scattering coefficient of aerosol particles measured with an integrating nephelometer during the Arctic haze period showed a distinct difference between the lower, i.e. up to around 4000 m, and higher troposphere. Meanwhile, scattering coefficients in higher troposphere during the Arctic haze were in the same degree with those after the Arctic haze. Size distribution obtained from the data of a particle counter indicates that aerosol particles in accumulation mode during the Arctic haze have larger geometric mean diameter than those after the haze season, which reflects the aged air mass in the Arctic haze. "Curtain flight" which was carried out to reveal the fine structure of the haze layer showed that aerosol particles are transported in the isentropic plane. |
format |
Article in Journal/Newspaper |
author |
Sadamu Yamagata Keiichiro Hara Atsushi Matsuki |
author_facet |
Sadamu Yamagata Keiichiro Hara Atsushi Matsuki |
author_sort |
Sadamu Yamagata |
title |
Scattering coefficient, size distribution and the transport process of tropospheric aerosol in the Arctic region observed with an aircraft during ASTAR 2000/2004 and AAMP 2002 campaign in spring |
title_short |
Scattering coefficient, size distribution and the transport process of tropospheric aerosol in the Arctic region observed with an aircraft during ASTAR 2000/2004 and AAMP 2002 campaign in spring |
title_full |
Scattering coefficient, size distribution and the transport process of tropospheric aerosol in the Arctic region observed with an aircraft during ASTAR 2000/2004 and AAMP 2002 campaign in spring |
title_fullStr |
Scattering coefficient, size distribution and the transport process of tropospheric aerosol in the Arctic region observed with an aircraft during ASTAR 2000/2004 and AAMP 2002 campaign in spring |
title_full_unstemmed |
Scattering coefficient, size distribution and the transport process of tropospheric aerosol in the Arctic region observed with an aircraft during ASTAR 2000/2004 and AAMP 2002 campaign in spring |
title_sort |
scattering coefficient, size distribution and the transport process of tropospheric aerosol in the arctic region observed with an aircraft during astar 2000/2004 and aamp 2002 campaign in spring |
publisher |
National Institute of Polar Research |
publishDate |
2010 |
url |
https://doi.org/10.15094/00009590 https://doaj.org/article/30cb2dfd6cdb4627b0f002511292e54e |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
Antarctic Record, Vol 54, Iss special issue, Pp 868-881 (2010) |
op_relation |
doi:10.15094/00009590 0085-7289 2432-079X https://doaj.org/article/30cb2dfd6cdb4627b0f002511292e54e |
op_rights |
undefined |
op_doi |
https://doi.org/10.15094/00009590 |
_version_ |
1766306193490313216 |