001     863786
005     20240712100907.0
020 _ _ |a 978-3-95806-404-1
024 7 _ |a 2128/22604
|2 Handle
037 _ _ |a FZJ-2019-03777
041 _ _ |a English
100 1 _ |a Khattatov, Talat
|0 P:(DE-Juel1)161490
|b 0
|e Corresponding author
|u fzj
245 _ _ |a Development, calibration and deployment of an airborne chemical ionization mass spectrometer for trace gas measurements
|f - 2019-08-20
260 _ _ |a Jülich
|c 2019
|b Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag
300 _ _ |a 14, 125
336 7 _ |a Output Types/Dissertation
|2 DataCite
336 7 _ |a Book
|0 PUB:(DE-HGF)3
|2 PUB:(DE-HGF)
|m book
336 7 _ |a DISSERTATION
|2 ORCID
336 7 _ |a PHDTHESIS
|2 BibTeX
336 7 _ |a Thesis
|0 2
|2 EndNote
336 7 _ |a Dissertation / PhD Thesis
|b phd
|m phd
|0 PUB:(DE-HGF)11
|s 1593419899_16974
|2 PUB:(DE-HGF)
336 7 _ |a doctoralThesis
|2 DRIVER
490 0 _ |a Schriften des Forschungszentrums Jülich Reihe Energie & Umwelt / Energy & Environment
|v 464
502 _ _ |a Dissertation, Univ. Wuppertal, 2019
|c Univ. Wuppertal
|b Dissertation
|d 2019
520 _ _ |a Some ultra trace gas species present in the upper troposphere and lower stratosphere(UTLS) region at low part-per-billion and part-per-trillion mixing ratios are known to havea major effect on atmospheric chemistry and climate. Chlorine and bromine species causingstrong ozone depletion and sulfur dioxide (SO$_{2}$) driving aerosol formation processes of high relevance to the global radiative budget are prominent examples. Nitric acid (HNO$_{3}$)is another species, which is quite important for particle formation and denitrification processes. In order to fully understand and reliably model the involved processes for climatepredictions, spatially highly resolved in-situ measurements of these species are needed. Therefore robust instruments are required that can perform very sensitive and accuratemeasurements of ultra-trace species in the extremely challenging UTLS environment from balloons or favorably high-flying aircraft, which impose stringent mechanical and electrical constraints. Here I describe the set-up, test, characterization, deployment, data analysis, and preliminary results of the new FunMass instrument tailored to the deployment on the high-flyingresearch aircraft M-55 Geophysica. FunMass utilizes the established techniques of chemical ionization mass spectrometry (CIMS) in an unprecedented package pairing measurementsensitivity and accuracy with high versatility at reasonable instrumental weight and dimensions. FunMass was set up based on a laboratory prototype [1]: the concept of its transferstage with an ion funnel and its dielectric barrier discharge (DBD) ion source was adapted for the airborne version of the instrument. The ion funnel improves the sensitivity of the instrument at least by one order of magnitude and the DBD ion source is an excellent replacement for the logistically very challenging radioactive ion source, which is widely used for CIMS. A big advantage of the TOF-MS technique for airborne measurements is that it is capable of fast and simultaneous acquisition of full mass spectra and therefore measurements of many different ion species, which is very important since flight hours of research aircraft are a very limited resource [...]
536 _ _ |a 244 - Composition and dynamics of the upper troposphere and middle atmosphere (POF3-244)
|0 G:(DE-HGF)POF3-244
|c POF3-244
|f POF III
|x 0
856 4 _ |u https://juser.fz-juelich.de/record/863786/files/Energie_Umwelt_464.pdf
|y OpenAccess
909 C O |o oai:juser.fz-juelich.de:863786
|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 0
|6 P:(DE-Juel1)161490
913 1 _ |a DE-HGF
|l Atmosphäre und Klima
|1 G:(DE-HGF)POF3-240
|0 G:(DE-HGF)POF3-244
|2 G:(DE-HGF)POF3-200
|v Composition and dynamics of the upper troposphere and middle atmosphere
|x 0
|4 G:(DE-HGF)POF
|3 G:(DE-HGF)POF3
|b Erde und Umwelt
914 1 _ |y 2019
915 _ _ |a OpenAccess
|0 StatID:(DE-HGF)0510
|2 StatID
915 _ _ |a Creative Commons Attribution CC BY 4.0
|0 LIC:(DE-HGF)CCBY4
|2 HGFVOC
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 phd
980 _ _ |a VDB
980 _ _ |a book
980 _ _ |a I:(DE-Juel1)IEK-7-20101013
980 _ _ |a UNRESTRICTED
981 _ _ |a I:(DE-Juel1)ICE-4-20101013


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