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@ARTICLE{Newman:23760,
author = {Newman, P. A. and Harris, R. J. and Adriani, A. and
Amanatidis, G. and Anderson, J. and Braathen, G. and Brune,
W. and Carslaw, K. and Craig, M. and de Cola, P. and
Guirlet, M. and Hipskind, S. and Kurylo, M. and Küllmann,
H. and Larsen, N. and Megie, G. and Pommereau, J. P. and
Poole, L. and Schoeber, M. and Stroh, F. and Toon, B. and
Trepte, C. and van Scheer, M.},
title = {{A}n overview of the {SOLVE}-{THESEO} 2000 campaign},
journal = {Journal of Geophysical Research},
volume = {107},
issn = {0148-0227},
address = {Washington, DC},
publisher = {Union},
reportid = {PreJuSER-23760},
pages = {D20},
year = {2002},
note = {Record converted from VDB: 12.11.2012},
abstract = {Between November 1999 and April 2000, two major field
experiments, the Stratospheric Aerosol and Gas Experiment
(SAGE) III Ozone Loss and Validation Experiment (SOLVE) and
the Third European Stratospheric Experiment on Ozone (THESEO
2000), collaborated to form the largest field campaign yet
mounted to study Arctic ozone loss. This international
campaign involved more than 500 scientists from over 20
countries. These scientists made measurements across the
high and middle latitudes of the Northern Hemisphere. The
main scientific aims of SOLVE/THESEO 2000 were to study (1)
the processes leading to ozone loss in the Arctic vortex and
(2) the effect on ozone amounts over northern midlatitudes.
The campaign included satellites, research balloons, six
aircraft, ground stations, and scores of ozonesondes.
Campaign activities were principally conducted in three
intensive measurement phases centered on early December
1999, late January 2000, and early March 2000. Observations
made during the campaign showed that temperatures were below
normal in the polar lower stratosphere over the course of
the 1999-2000 winter. Because of these low temperatures,
extensive polar stratospheric clouds (PSC) formed across the
Arctic. Large particles containing nitric acid trihydrate
were observed for the first time, showing that
denitrification can occur without the formation of ice
particles. Heterogeneous chemical reactions on the surfaces
of the PSC particles produced high levels of reactive
chlorine within the polar vortex by early January. This
reactive chlorine catalytically destroyed about $60\%$ of
the ozone in a layer near 20 km between late January and
mid-March 2000, with good agreement being found between a
number of empirical and modeling studies. The measurements
made during SOLVE/THESEO 2000 have improved our
understanding of key photochemical parameters and the
evolution of ozone-destroying forms of chlorine.},
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:000180466200105},
doi = {10.1029/2001JD001303},
url = {https://juser.fz-juelich.de/record/23760},
}