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@PHDTHESIS{SuminskaEbersoldt:22872,
author = {Suminska-Ebersoldt, Olga},
title = {{S}tratospheric {C}l{OOC}l chemistry at high solar zenith
angles},
volume = {151},
school = {Universität Wuppertal},
type = {Dr.},
address = {Jülich},
publisher = {Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag},
reportid = {PreJuSER-22872},
isbn = {978-3-89336-817-4},
series = {Schriften des Forschungszentrums Jülich : Energie $\&$
Umwelt / Energy $\&$ Environment},
pages = {VI, 126 S.},
year = {2012},
note = {Record converted from JUWEL: 18.07.2013; Universität
Wuppertal, Diss., 2012},
abstract = {The photolysis rate constant of dichlorine peroxide
(ClOOCl, ClO dimer), J$_{ClOOCl}$, is a critical parameter
in catalytic cycles destroying ozone (O$_{3}$) in the polar
stratosphere. In the atmospherically relevant wavelength
region (310 – 500 nm), significant discrepancies between
laboratory measurements of ClOOCl absorption cross sections
and spectra cause a large uncertainty in J$_{ClOOCl}$.
Previous investigations of the consistency of published
J$_{ClOOCl}$ with atmospheric observations of chlorine
monoxide (ClO) and ClOOCl have focused on the photochemical
equilibrium between ClOOCl formation and photolysis, and
thus could only constrain the ratio of J$_{ClOOCl}$ and the
ClOOCl formation rate constant k$_{rec}$. Here, the
atmospherically effective J$_{ClOOCl}$ was constrained
independent of krec, using ClO measured in the same air
masses before and directly after sunrise during an aircraft
flight that was carried out as a part of the RECONCILE field
campaign in winter 2010 over Kiruna, Sweden. Over sunrise,
when the ClO/ClOOCl system comes out of thermal equilibrium,
the influence of the ClO recombination reaction is
negligible and the ClO concentration increase results from
the photolysis of ClOOCl. J$_{ClOOCl}$ values based on four
absorption cross sections and spectra were estimated for the
atmospheric conditions on the flight track and resulting ClO
concentration increases were compared with the observed ClO
rise. The analysis shows, that the increase in measured ClO
concentrations was significantly faster than expected from
J$_{ClOOCl}$ based on the absorption spectrum proposed by
Pope et al. (2007), but did not warrant cross sections
larger than recently published values by Papanastasiou et
al. (2009). In particular, the existence of a significant
ClOOCl absorption band longwards of 420nm is not supported
by the observations. The observed night-time ClO is not
consistent with a ClO/ClOOCl thermal equilibrium constant
significantly higher [...]},
cin = {IEK-7},
ddc = {500},
cid = {I:(DE-Juel1)IEK-7-20101013},
pnm = {Atmosphäre und Klima},
pid = {G:(DE-Juel1)FUEK491},
typ = {PUB:(DE-HGF)11 / PUB:(DE-HGF)3},
url = {https://juser.fz-juelich.de/record/22872},
}