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@ARTICLE{Groo:16556,
author = {Grooß, J.-U. and Günther, G. and Konopka, Paul and
Müller, R. and McKenna, D. S. and Stroh, F. and Vogel, B.
and Engel, A. and Müller, M. and Hoppel, K. and Bevilacqua,
R. and Richard, E. and Webster, C. R. and Elkins, J. W. and
Hurst, D. F. and Roamshkin, P. A. and Baumgardner, D. G.},
title = {{S}imulation of ozone depletion in spring 2000 with the
{C}hemical {L}agrangian {M}odel of the {S}tratosphere
({CL}a{MS})},
journal = {Journal of Geophysical Research},
volume = {107},
issn = {0148-0227},
address = {Washington, DC},
publisher = {Union},
reportid = {PreJuSER-16556},
year = {2002},
note = {Record converted from VDB: 12.11.2012},
abstract = {Simulations of the development of the chemical composition
of the Arctic stratosphere for spring 2000 are made with the
Chemical Lagrangian Model of the Stratosphere (CLaMS). The
simulations are performed for the entire Northern Hemisphere
on four isentropic levels (400-475 K). The initialization in
early February is based on observations made from satellite,
balloon and ER-2 aircraft platforms. Tracer-tracer
correlations from balloon-borne cryosampler (Triple) and
ER-2 measurements, as well as tracer-PV correlations, are
used to derive a comprehensive hemispherical initialization
of all relevant chemical trace species. Since significant
denitrification has been observed on the ER-2 flights, a
parameterization of the denitrification is derived from NOy
and N2O observations on board the ER-2 aircraft and the
temperature history of the air masses under consideration.
Over the simulation period from 10 February to 20 March, a
chemical ozone depletion of up to $60\%$ was derived for
425-450 K potential temperature. Maximum vortex-averaged
chemical ozone loss rates of 50 ppb d(-1) or 4 ppb per
sunlight hour were simulated in early March 2000 at the 425
and 450 K potential temperature levels. We show comparisons
between the measurements and the simulations for the
location of the ER-2 flight paths in late February and March
and the location of the Triple balloon flight. The simulated
tracer mixing ratios are in good agreement with the
measurements. It was not possible to reproduce the exact
details of the inorganic chlorine compounds. The simulation
agrees with ClOx observations on the Triple balloon flight
but overestimates for the ER-2 flights. The simulated ozone
depletion agrees with estimates from other observations in
the 425 and 450 K levels, but is underestimated on the 475 K
level.},
keywords = {J (WoSType)},
cin = {ICG-I},
ddc = {550},
cid = {I:(DE-Juel1)VDB47},
pnm = {Chemie und Dynamik der Geo-Biosphäre},
pid = {G:(DE-Juel1)FUEK257},
shelfmark = {Meteorology $\&$ Atmospheric Sciences},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000180466200092},
doi = {10.1029/2001JD000456},
url = {https://juser.fz-juelich.de/record/16556},
}