A meteorological overview of the ARCTAS 2008 mission

The A rctic R esearch of the C omposition of the T roposphere from A ircraft and S atellites (ARCTAS) mission was a multi-aircraft project whose major objective was to investigate the factors driving changes in the Arctic's atmospheric composition and climate. It was conducted during April and...

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Main Authors: H. E. Fuelberg, D. L. Harrigan, W. Sessions
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2010
Subjects:
Online Access:https://doaj.org/article/4f00cae998084201a5a9ba979c9b7464
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spelling ftdoajarticles:oai:doaj.org/article:4f00cae998084201a5a9ba979c9b7464 2023-05-15T14:59:49+02:00 A meteorological overview of the ARCTAS 2008 mission H. E. Fuelberg D. L. Harrigan W. Sessions 2010-01-01T00:00:00Z https://doaj.org/article/4f00cae998084201a5a9ba979c9b7464 EN eng Copernicus Publications http://www.atmos-chem-phys.net/10/817/2010/acp-10-817-2010.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 1680-7316 1680-7324 https://doaj.org/article/4f00cae998084201a5a9ba979c9b7464 Atmospheric Chemistry and Physics, Vol 10, Iss 2, Pp 817-842 (2010) Physics QC1-999 Chemistry QD1-999 article 2010 ftdoajarticles 2022-12-31T03:00:09Z The A rctic R esearch of the C omposition of the T roposphere from A ircraft and S atellites (ARCTAS) mission was a multi-aircraft project whose major objective was to investigate the factors driving changes in the Arctic's atmospheric composition and climate. It was conducted during April and June–July 2008. The summer ARCTAS deployment was preceded by a week of flights over and around California to address state issues of air quality and climate forcing. This paper focuses on meteorological conditions during the ARCTAS Spring and Summer campaigns. We examine mission averaged large-scale flow patterns at the surface, 500 hPa, and 300 hPa and determine their departures from climatology. Results from runs of the W eather R esearch and F orecasting (WRF) model are used to describe meteorological conditions on individual days. Our WRF configuration included a nested grid approach that provided horizontal spacing as small as 5 km. Trajectories calculated from the WRF output are used to determine transport pathways to the Arctic, including their origins and the altitudes at which they reach 70° N. We also present backward trajectories from selected legs of individual ARCTAS flights. Finally, the FLEXPART Lagrangian particle dispersion model, with the high resolution WRF data as input, is used to determine the paths of anthropogenic and biomass burning-derived CO. Results show that there was frequent and widespread transport to the Arctic during both phases of ARCTAS and that the three ARCTAS aircraft sampled air having a multitude of origins, following a myriad of paths, and experiencing many types of meteorological conditions. Article in Journal/Newspaper Arctic Directory of Open Access Journals: DOAJ Articles Arctic Eather ENVELOPE(65.833,65.833,-70.483,-70.483)
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Physics
QC1-999
Chemistry
QD1-999
spellingShingle Physics
QC1-999
Chemistry
QD1-999
H. E. Fuelberg
D. L. Harrigan
W. Sessions
A meteorological overview of the ARCTAS 2008 mission
topic_facet Physics
QC1-999
Chemistry
QD1-999
description The A rctic R esearch of the C omposition of the T roposphere from A ircraft and S atellites (ARCTAS) mission was a multi-aircraft project whose major objective was to investigate the factors driving changes in the Arctic's atmospheric composition and climate. It was conducted during April and June–July 2008. The summer ARCTAS deployment was preceded by a week of flights over and around California to address state issues of air quality and climate forcing. This paper focuses on meteorological conditions during the ARCTAS Spring and Summer campaigns. We examine mission averaged large-scale flow patterns at the surface, 500 hPa, and 300 hPa and determine their departures from climatology. Results from runs of the W eather R esearch and F orecasting (WRF) model are used to describe meteorological conditions on individual days. Our WRF configuration included a nested grid approach that provided horizontal spacing as small as 5 km. Trajectories calculated from the WRF output are used to determine transport pathways to the Arctic, including their origins and the altitudes at which they reach 70° N. We also present backward trajectories from selected legs of individual ARCTAS flights. Finally, the FLEXPART Lagrangian particle dispersion model, with the high resolution WRF data as input, is used to determine the paths of anthropogenic and biomass burning-derived CO. Results show that there was frequent and widespread transport to the Arctic during both phases of ARCTAS and that the three ARCTAS aircraft sampled air having a multitude of origins, following a myriad of paths, and experiencing many types of meteorological conditions.
format Article in Journal/Newspaper
author H. E. Fuelberg
D. L. Harrigan
W. Sessions
author_facet H. E. Fuelberg
D. L. Harrigan
W. Sessions
author_sort H. E. Fuelberg
title A meteorological overview of the ARCTAS 2008 mission
title_short A meteorological overview of the ARCTAS 2008 mission
title_full A meteorological overview of the ARCTAS 2008 mission
title_fullStr A meteorological overview of the ARCTAS 2008 mission
title_full_unstemmed A meteorological overview of the ARCTAS 2008 mission
title_sort meteorological overview of the arctas 2008 mission
publisher Copernicus Publications
publishDate 2010
url https://doaj.org/article/4f00cae998084201a5a9ba979c9b7464
long_lat ENVELOPE(65.833,65.833,-70.483,-70.483)
geographic Arctic
Eather
geographic_facet Arctic
Eather
genre Arctic
genre_facet Arctic
op_source Atmospheric Chemistry and Physics, Vol 10, Iss 2, Pp 817-842 (2010)
op_relation http://www.atmos-chem-phys.net/10/817/2010/acp-10-817-2010.pdf
https://doaj.org/toc/1680-7316
https://doaj.org/toc/1680-7324
1680-7316
1680-7324
https://doaj.org/article/4f00cae998084201a5a9ba979c9b7464
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