001     892875
005     20240712100919.0
024 7 _ |a 10.5194/acp-21-8213-2021
|2 doi
024 7 _ |a 1680-7316
|2 ISSN
024 7 _ |a 1680-7324
|2 ISSN
024 7 _ |a 2128/27871
|2 Handle
024 7 _ |a altmetric:106500408
|2 altmetric
024 7 _ |a WOS:000657177200005
|2 WOS
037 _ _ |a FZJ-2021-02414
082 _ _ |a 550
100 1 _ |a Wetzel, Gerald
|0 P:(DE-HGF)0
|b 0
|e Corresponding author
245 _ _ |a Pollution trace gases C2H6, C2H2, HCOOH, and PAN in the North Atlantic UTLS: observations and simulations
260 _ _ |a Katlenburg-Lindau
|c 2021
|b EGU
336 7 _ |a article
|2 DRIVER
336 7 _ |a Output Types/Journal article
|2 DataCite
336 7 _ |a Journal Article
|b journal
|m journal
|0 PUB:(DE-HGF)16
|s 1669887838_20109
|2 PUB:(DE-HGF)
336 7 _ |a ARTICLE
|2 BibTeX
336 7 _ |a JOURNAL_ARTICLE
|2 ORCID
336 7 _ |a Journal Article
|0 0
|2 EndNote
520 _ _ |a Measurements of the pollution trace gases ethane (C2H6), ethyne (C2H2), formic acid (HCOOH), and peroxyacetyl nitrate (PAN) were performed in the North Atlantic upper troposphere and lowermost stratosphere (UTLS) region with the airborne limb imager GLORIA (Gimballed Limb Observer for Radiance Imaging of the Atmosphere) with high spatial resolution down to cloud top. Observations were made during flights with the German research aircraft HALO (High Altitude and LOng Range Research Aircraft) in the frame of the WISE (Wave-driven ISentropic Exchange) campaign, which was carried out in autumn 2017 from Shannon (Ireland) and Oberpfaffenhofen (Germany). Enhanced volume mixing ratios (VMRs) of up to 2.2 ppbv C2H6, 0.2 ppbv C2H2, 0.9 ppbv HCOOH, and 0.4 ppbv PAN were detected during the flight on 13 September 2017 in the upper troposphere and around the tropopause above the British Isles. Elevated quantities of PAN were measured even in the lowermost stratosphere (locally up to 14 km), likely reflecting the fact that this molecule has the longest lifetime of the four species discussed herein. Backward trajectory calculations as well as global three-dimensional Chemical Lagrangian Model of the Stratosphere (CLaMS) simulations with artificial tracers of air mass origin have shown that the main sources of the observed pollutant species are forest fires in North America and anthropogenic pollution in South Asia and Southeast Asia uplifted and moved within the Asian monsoon anticyclone (AMA) circulation system. After release from the AMA, these species or their precursor substances are transported by strong tropospheric winds over large distances, depending on their particular atmospheric lifetime of up to months. Observations are compared to simulations with the atmospheric models EMAC (ECHAM5/MESSy Atmospheric Chemistry) and CAMS (Copernicus Atmosphere Monitoring Service). These models are qualitatively able to reproduce the measured VMR enhancements but underestimate the absolute amount of the increase. Increasing the emissions in EMAC by a factor of 2 reduces the disagreement between simulated and measured results and illustrates the importance of the quality of emission databases used in chemical models.
536 _ _ |a 211 - Die Atmosphäre im globalen Wandel (POF4-211)
|0 G:(DE-HGF)POF4-211
|c POF4-211
|f POF IV
|x 0
536 _ _ |a 2A3 - Remote Sensing (CARF - CCA) (POF4-2A3)
|0 G:(DE-HGF)POF4-2A3
|c POF4-2A3
|f POF IV
|x 1
588 _ _ |a Dataset connected to CrossRef, Journals: juser.fz-juelich.de
700 1 _ |a Friedl-Vallon, Felix
|0 0000-0003-2016-2800
|b 1
700 1 _ |a Glatthor, Norbert
|0 P:(DE-HGF)0
|b 2
700 1 _ |a Grooß, Jens-Uwe
|0 P:(DE-Juel1)129122
|b 3
700 1 _ |a Gulde, Thomas
|0 P:(DE-HGF)0
|b 4
700 1 _ |a Höpfner, Michael
|0 0000-0002-4174-9531
|b 5
700 1 _ |a Johansson, Sören
|0 0000-0002-9642-1955
|b 6
700 1 _ |a Khosrawi, Farahnaz
|0 0000-0002-0261-7253
|b 7
700 1 _ |a Kirner, Oliver
|0 P:(DE-HGF)0
|b 8
700 1 _ |a Kleinert, Anne
|0 P:(DE-HGF)0
|b 9
700 1 _ |a Kretschmer, Erik
|0 0000-0001-8923-5516
|b 10
700 1 _ |a Maucher, Guido
|0 P:(DE-HGF)0
|b 11
700 1 _ |a Nordmeyer, Hans
|0 P:(DE-HGF)0
|b 12
700 1 _ |a Oelhaf, Hermann
|0 P:(DE-HGF)0
|b 13
700 1 _ |a Orphal, Johannes
|0 P:(DE-HGF)0
|b 14
700 1 _ |a Piesch, Christof
|0 P:(DE-HGF)0
|b 15
700 1 _ |a Sinnhuber, Björn-Martin
|0 0000-0001-9608-7320
|b 16
700 1 _ |a Ungermann, Jörn
|0 P:(DE-Juel1)129105
|b 17
700 1 _ |a Vogel, Bärbel
|0 P:(DE-Juel1)129164
|b 18
773 _ _ |a 10.5194/acp-21-8213-2021
|g Vol. 21, no. 10, p. 8213 - 8232
|0 PERI:(DE-600)2069847-1
|n 10
|p 8213 - 8232
|t Atmospheric chemistry and physics
|v 21
|y 2021
|x 1680-7324
856 4 _ |u https://juser.fz-juelich.de/record/892875/files/acp-21-8213-2021.pdf
|y OpenAccess
909 C O |o oai:juser.fz-juelich.de:892875
|p openaire
|p open_access
|p driver
|p VDB:Earth_Environment
|p VDB
|p dnbdelivery
910 1 _ |a Forschungszentrum Jülich
|0 I:(DE-588b)5008462-8
|k FZJ
|b 3
|6 P:(DE-Juel1)129122
910 1 _ |a Forschungszentrum Jülich
|0 I:(DE-588b)5008462-8
|k FZJ
|b 17
|6 P:(DE-Juel1)129105
910 1 _ |a Forschungszentrum Jülich
|0 I:(DE-588b)5008462-8
|k FZJ
|b 18
|6 P:(DE-Juel1)129164
913 1 _ |a DE-HGF
|b Forschungsbereich Erde und Umwelt
|l Erde im Wandel – Unsere Zukunft nachhaltig gestalten
|1 G:(DE-HGF)POF4-210
|0 G:(DE-HGF)POF4-211
|3 G:(DE-HGF)POF4
|2 G:(DE-HGF)POF4-200
|4 G:(DE-HGF)POF
|v Die Atmosphäre im globalen Wandel
|x 0
913 1 _ |a DE-HGF
|b Forschungsbereich Erde und Umwelt
|l COOPERATION ACROSS RESEARCH FIELDS (CARFs)
|1 G:(DE-HGF)POF4-2A0
|0 G:(DE-HGF)POF4-2A3
|3 G:(DE-HGF)POF4
|2 G:(DE-HGF)POF4-200
|4 G:(DE-HGF)POF
|v Remote Sensing (CARF - CCA)
|x 1
913 0 _ |a DE-HGF
|b Erde und Umwelt
|l Atmosphäre und Klima
|1 G:(DE-HGF)POF3-240
|0 G:(DE-HGF)POF3-244
|3 G:(DE-HGF)POF3
|2 G:(DE-HGF)POF3-200
|4 G:(DE-HGF)POF
|v Composition and dynamics of the upper troposphere and middle atmosphere
|x 0
914 1 _ |y 2021
915 _ _ |a DBCoverage
|0 StatID:(DE-HGF)0200
|2 StatID
|b SCOPUS
|d 2021-02-02
915 _ _ |a DBCoverage
|0 StatID:(DE-HGF)0160
|2 StatID
|b Essential Science Indicators
|d 2021-02-02
915 _ _ |a Creative Commons Attribution CC BY 4.0
|0 LIC:(DE-HGF)CCBY4
|2 HGFVOC
915 _ _ |a DBCoverage
|0 StatID:(DE-HGF)1150
|2 StatID
|b Current Contents - Physical, Chemical and Earth Sciences
|d 2021-02-02
915 _ _ |a IF >= 5
|0 StatID:(DE-HGF)9905
|2 StatID
|b ATMOS CHEM PHYS : 2019
|d 2021-02-02
915 _ _ |a DBCoverage
|0 StatID:(DE-HGF)0501
|2 StatID
|b DOAJ Seal
|d 2021-02-02
915 _ _ |a DBCoverage
|0 StatID:(DE-HGF)0500
|2 StatID
|b DOAJ
|d 2021-02-02
915 _ _ |a WoS
|0 StatID:(DE-HGF)0113
|2 StatID
|b Science Citation Index Expanded
|d 2021-02-02
915 _ _ |a Fees
|0 StatID:(DE-HGF)0700
|2 StatID
|d 2021-02-02
915 _ _ |a DBCoverage
|0 StatID:(DE-HGF)0150
|2 StatID
|b Web of Science Core Collection
|d 2021-02-02
915 _ _ |a OpenAccess
|0 StatID:(DE-HGF)0510
|2 StatID
915 _ _ |a Peer Review
|0 StatID:(DE-HGF)0030
|2 StatID
|b DOAJ : Peer review
|d 2021-02-02
915 _ _ |a Article Processing Charges
|0 StatID:(DE-HGF)0561
|2 StatID
|d 2021-02-02
915 _ _ |a JCR
|0 StatID:(DE-HGF)0100
|2 StatID
|b ATMOS CHEM PHYS : 2019
|d 2021-02-02
915 _ _ |a DBCoverage
|0 StatID:(DE-HGF)0300
|2 StatID
|b Medline
|d 2021-02-02
915 _ _ |a DBCoverage
|0 StatID:(DE-HGF)0199
|2 StatID
|b Clarivate Analytics Master Journal List
|d 2021-02-02
920 _ _ |l yes
920 1 _ |0 I:(DE-Juel1)IEK-7-20101013
|k IEK-7
|l Stratosphäre
|x 0
980 1 _ |a FullTexts
980 _ _ |a journal
980 _ _ |a VDB
980 _ _ |a I:(DE-Juel1)IEK-7-20101013
980 _ _ |a UNRESTRICTED
981 _ _ |a I:(DE-Juel1)ICE-4-20101013


LibraryCollectionCLSMajorCLSMinorLanguageAuthor
Marc 21