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@ARTICLE{Wang:22838,
author = {Wang, Y. and Konopka, P. and Liu, Y. and Chen, H. and
Müller, R. and Plöger, F. and Riese, M. and Cai, Z. and
Lü, D.},
title = {{T}ropospheric ozone trend over {B}eijing from 2001-2010:
ozonesonde measurements and modeling analysis},
journal = {Atmospheric chemistry and physics},
volume = {12},
issn = {1680-7316},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {PreJuSER-22838},
pages = {8389 - 8399},
year = {2012},
note = {This work was funded by the National Basic Research Program
of China (grant 2010CB428604), the National Science
Foundation of China (grant 41075014 and 40830102) and the
PhD program of Forschungszentrum Julich. We thank Gengchen
Wang, Yuejian Xuan, Xiaowei Wan and Jianchun Bian for their
contributions to Beijing ozonesonde observation. We thank
J.-U. Grooss and A. Kunz for their very helpful comments.
The European Centre for Medium-Range Weather Forecasts
(ECMWF) is acknowledged for meteorological data support. We
thank NASA (National Aeronautics and Space Administration)
earth data website and Institute of Environmental Physics,
University of Bremen for supplying the total ozone data.},
abstract = {Using a combination of ozonesonde data and numerical
simulations of the Chemical Lagrangian Model of the
Stratosphere (CLaMS), the trend of tropospheric ozone (O-3)
during 2002-2010 over Beijing was investigated. Tropospheric
ozone over Beijing shows a winter minimum and a broad summer
maximum with a clear positive trend in the maximum summer
ozone concentration over the last decade. The observed
significant trend of tropospheric column ozone is mainly
caused by photochemical production $(3.1\%$ yr(-1) for a
mean level of 52 DU). This trend is close to the significant
trend of partial column ozone in the lower troposphere (0-3
km) resulting from the enhanced photochemical production
during summer $(3.0\%$ yr(-1) for a mean level of 23 DU).
Analysis of the CLaMS simulation shows that transport rather
than chemistry drives most of the seasonality of
tropospheric ozone. However, dynamical processes alone
cannot explain the trend of tropospheric ozone in the
observational data. Clearly enhanced ozone values and a
negative vertical ozone gradient in the lower troposphere in
the observational data emphasize the importance of
photochemistry within the troposphere during spring and
summer, and suggest that the photochemistry within the
troposphere significantly contributes to the tropospheric
ozone trend over Beijing during the last decade.},
keywords = {J (WoSType)},
cin = {IEK-7},
ddc = {550},
cid = {I:(DE-Juel1)IEK-7-20101013},
pnm = {Atmosphäre und Klima},
pid = {G:(DE-Juel1)FUEK491},
shelfmark = {Meteorology $\&$ Atmospheric Sciences},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000309424300006},
doi = {10.5194/acp-12-8389-2012},
url = {https://juser.fz-juelich.de/record/22838},
}