001     910209
005     20240712100847.0
020 _ _ |a 978-3-95806-648-9
024 7 _ |a 2128/32116
|2 Handle
037 _ _ |a FZJ-2022-03686
100 1 _ |a Khordakova, Dina
|0 P:(DE-Juel1)173706
|b 0
|e Corresponding author
|u fzj
245 _ _ |a Impact of severe convection on the water vapor mixing ratio in the extra-tropical stratosphere
|f - 2022-10-26
260 _ _ |a Jülich
|c 2022
|b Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag
300 _ _ |a ii, 136
336 7 _ |a Output Types/Dissertation
|2 DataCite
336 7 _ |a Book
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336 7 _ |a DISSERTATION
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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 1666772911_6245
|2 PUB:(DE-HGF)
336 7 _ |a doctoralThesis
|2 DRIVER
490 0 _ |a Schriften des Forschungszentrums Jülich Reihe Energie & Umwelt / Energy & Environment
|v 586
502 _ _ |a Dissertation, Wuppertal, 2022
|c Wuppertal
|b Dissertation
|d 2022
520 _ _ |a The emission of anthropogenic greenhouse gases leads to a continuous increase in average global surface temperatures. The radiative effect of the anthropogenic sources is amplified by feedback processes, like the water vapor feedback. The rapid change in climatic conditions is evident not only in the mean of the relevant weather parameters, but also in the severity and frequency of extreme events. Extreme convective events in the troposphere not only have immediate impacts on the surface, they can also influence the dynamics and composition of the stratosphere. One major impact is the moistening of the stratosphere by the transport of tropospheric air masses by overshooting convection and pyro-convection. This effect plays a crucial role in climate feedback as small changes of water vapor mixing ratios in the upper troposphere and lower stratosphere (UTLS) have a large impact on the radiative budget of the atmosphere and hence have an additional positive feedback on the changing climate. In this thesis four cases are investigated in which water vapor was injected into the stratosphere. Two of them are cases of convective overshooting and two are cases of pyro-convection. In all of these cases, unusual values of water vapor were measured in the stratosphere and a persistent dynamical signature (potential vorticity anomaly) was produced. For the convective case, the measurements were made by the Cryogenic Frostpoint Hygrometer (CFH) which requires Triflouromethane (R-23) as a cooling agent. Since the year 2020, R-23 has not been acquirable in Europe. Hence, an alternative cooling method for the instrument was successfully explored and tested. The two cases of convective overshooting were investigated on two consecutive days in the European mid-latitudes in early summer of 2019. Using balloon-borne instruments, measurements of convectively injected water vapor in the stratosphere were performed. The magnitude of the affected stratospheric water vapor reached up to 12.1 ppmv with an estimated background value of 5 ppmv. The corresponding water vapor values measured by the Microwave Limb Sounder (MLS) satellite in the lower stratosphere (LS) are lower than the in-situ observations and the fifth generation of ECMWF atmospheric global reanalysis (ERA5) reanalysis overestimated water vapor mixing ratios.
536 _ _ |a 2112 - Climate Feedbacks (POF4-211)
|0 G:(DE-HGF)POF4-2112
|c POF4-211
|f POF IV
|x 0
856 4 _ |u https://juser.fz-juelich.de/record/910209/files/Energie_Umwelt_586.pdf
|y OpenAccess
909 C O |o oai:juser.fz-juelich.de:910209
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910 1 _ |a Forschungszentrum Jülich
|0 I:(DE-588b)5008462-8
|k FZJ
|b 0
|6 P:(DE-Juel1)173706
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
|9 G:(DE-HGF)POF4-2112
|x 0
914 1 _ |y 2022
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 UNRESTRICTED
980 _ _ |a book
980 _ _ |a I:(DE-Juel1)IEK-7-20101013
981 _ _ |a I:(DE-Juel1)ICE-4-20101013


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