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@ARTICLE{Katragkou:256352,
author = {Katragkou, E. and Zanis, P. and Tsikerdekis, A. and
Kapsomenakis, J. and Melas, D. and Eskes, H. and Flemming,
J. and Huijnen, V. and Inness, A. and Schultz, Martin and
Stein, O. and Zerefos, C. S.},
title = {{E}valuation of near-surface ozone over {E}urope from the
{MACC} reanalysis},
journal = {Geoscientific model development},
volume = {8},
number = {7},
issn = {1991-9603},
address = {Katlenburg-Lindau},
publisher = {Copernicus},
reportid = {FZJ-2015-06311},
pages = {2299 - 2314},
year = {2015},
abstract = {This work is an extended evaluation of near-surface ozone
as part of the global reanalysis of atmospheric composition,
produced within the European-funded project MACC (Monitoring
Atmospheric Composition and Climate). It includes an
evaluation over the period 2003–2012 and provides an
overall assessment of the modeling system performance with
respect to near-surface ozone for specific European
subregions. Measurements at rural locations from the
European Monitoring and Evaluation Program (EMEP) and the
European Air Quality Database (AirBase) were used for the
evaluation assessment. The fractional gross error of
near-surface ozone reanalysis is on average 24 $\%$ over
Europe, the highest found over Scandinavia (27 $\%)$ and the
lowest over the Mediterranean marine stations (21 $\%).$
Near-surface ozone shows mostly a negative bias in winter
and a positive bias during warm months. Assimilation reduces
the bias in near-surface ozone in most of the European
subregions – with the exception of Britain and Ireland and
the Iberian Peninsula and its impact is mostly notable in
winter. With respect to the seasonal cycle, the MACC
reanalysis reproduces the photochemically driven broad
spring-summer maximum of surface ozone of central and south
Europe. However, it does not capture adequately the early
spring peak and the shape of the seasonality at northern and
north-eastern Europe. The diurnal range of surface ozone,
which is as an indication of the local photochemical
production processes, is reproduced fairly well, with a
tendency for a small overestimation during the warm months
for most subregions (especially in central and southern
Europe). Possible reasons leading to discrepancies between
the MACC reanalysis and observations are discussed.},
cin = {IEK-8 / JSC},
ddc = {910},
cid = {I:(DE-Juel1)IEK-8-20101013 / I:(DE-Juel1)JSC-20090406},
pnm = {211 - Global Processes: Integrated Monitoring and Modelling
(POF3-211) / 511 - Computational Science and Mathematical
Methods (POF3-511) / MACC-III - Monitoring Atmospheric
Composition and Climate -III (633080) / 243 - Tropospheric
trace substances and their transformation processes
(POF3-243)},
pid = {G:(DE-HGF)POF3-211 / G:(DE-HGF)POF3-511 /
G:(EU-Grant)633080 / G:(DE-HGF)POF3-243},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000358917100022},
doi = {10.5194/gmd-8-2299-2015},
url = {https://juser.fz-juelich.de/record/256352},
}