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@ARTICLE{Lu:9338,
author = {Lu, K. and Zhang, Y. and Su, H. and Brauers, T. and Chou,
C.C. and Hofzumahaus, A. and Liu, S.C. and Kita, K. and
Kondo, Y. and Shao, M. and Wahner, A. and Wang, J. and Wang,
X. and Zhu, T.},
title = {{O}xidant ({O}3 + {NO}2) production processes and formation
regimes in {B}eijing},
journal = {Journal of Geophysical Research},
volume = {115},
issn = {0148-0227},
address = {Washington, DC},
publisher = {Union},
reportid = {PreJuSER-9338},
pages = {1 - 18},
year = {2010},
note = {This work was supported by the National Natural Science
Foundation of China (no. 40675072), the Ministry of Science
and Technology of China (2002CB410801), and the Beijing
Council of Science and Technology (HB200504-6 and no.
HB200504-2). The authors would like to thank the
CareBeijing-2006 team, especially M. Hu, L. M. Zeng, Z. M.
Chen, F. Holland, Y. F. Cheng, X. Li, and S. R. Lou, for
technical help and support at the field sites and F. Rohrer
for help in IDL programming. We are grateful to the
anonymous reviewers for their helpful comments on the
manuscript.},
abstract = {For CareBeijing-2006, two sites were established in urban
and suburban regions of Beijing in summer 2006. Observations
of O-3 and its precursors together with meteorological
parameters at both sites are presented. Gross ozone
production rate P(O-3) and sensitivity to nitric oxides
(NOx) and volatile organic compounds (VOCs) were
investigated using an observation-based photochemical box
model (OBM). P(O-3) varied from nearly zero to 120 and 50
ppb h(-1) for urban and suburban sites, respectively. These
rates were greater than the accumulation rates of the
observed oxidant (O-3 + NO2) concentrations. The O-3
episodes typically appeared under southerly wind conditions
with high P(O-3), especially at the urban site. Sensitivity
studies with and without measured nitrous acid (HONO) as a
model constraint suggested that the estimated P(O-3) at both
sites was strongly enhanced by radical production from HONO
photolysis. Both NOx- and VOC-sensitive chemistries existed
over time scales from hours to days at the two sites. The
variation in O-3-sensitive chemistry was relatively well
explained by the ratio of the average daytime total VOC
reactivity (k(TVOC)) to NO, with the transition chemistry
corresponding to a k(TVOC)/NO value of 2-4 s(-1) ppb(-1).
Pronounced diurnal variations in the O-3 production regime
were found. In the morning, conditions were always strongly
VOC-limited, while in the afternoon, conditions were
variable for different days and different sites. The
model-calculated results were tested by measurements of
H2O2, HNO3, total OH reactivity, and HOx radicals. The OBM
was generally capable of correctly simulating the levels of
P(O-3), although it might tend to overpredict the
VOC-sensitive chemistry.},
keywords = {J (WoSType)},
cin = {ICG-2},
ddc = {550},
cid = {I:(DE-Juel1)VDB791},
pnm = {Atmosphäre und Klima},
pid = {G:(DE-Juel1)FUEK406},
shelfmark = {Meteorology $\&$ Atmospheric Sciences},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000285585200003},
doi = {10.1029/2009JD012714},
url = {https://juser.fz-juelich.de/record/9338},
}