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@ARTICLE{Lou:12502,
author = {Lou, S. and Holland, F. and Rohrer, F. and Lu, K. and Bohn,
B. and Brauers, T. and Chang, C.C. and Fuchs, H. and
Häseler, R. and Kita, K. and Kondo, Y. and Li, X. and Shao,
M. and Zeng, L. and Wahner, A. and Zhang, Y. and Wang, W.
and Hofzumahaus, A.},
title = {{A}tmospheric {OH} reactivities in the {P}earl {R}iver
{D}elta - {C}hina in summer 2006: measurement and model
results},
journal = {Atmospheric chemistry and physics},
volume = {10},
issn = {1680-7316},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {PreJuSER-12502},
pages = {11243 - 11260},
year = {2010},
note = {We thank the PRiDe PRD2006 campaign team (2002CB410801),
especially M. Hu, N. Takegawa, and A. Oebel for help and
support at the field site. We thank Pinhua Xie, Anhui
Institute of Optics and Fine Mechanics in Hefei, China, for
providing the methane data. C. C. thanks Academic Sinica,
Taiwan, for financial support of this work.},
abstract = {Total atmospheric OH reactivities (k(OH)) have been
measured as reciprocal OH lifetimes by a newly developed
instrument at a rural site in the densely populated Pearl
River Delta (PRD) in Southern China in summer 2006. The
deployed technique, LP-LIF, uses laser flash photolysis (LP)
for artificial OH generation and laser-induced fluorescence
(LIF) to measure the time-dependent OH decay in samples of
ambient air. The reactivities observed at PRD covered a
range from 10 s(-1) to 120 s(-1), indicating a large load of
chemical reactants. On average, k(OH) exhibited a pronounced
diurnal profile with a mean maximum value of 50 s(-1) at
daybreak and a mean minimum value of 20 s(-1) at noon. The
comparison of reactivities calculated from measured trace
gases with measured k(OH) reveals a missing reactivity of
about a factor of 2 at day and night. The reactivity
explained by measured trace gases was dominated by
anthropogenic pollutants (e. g., CO, NOx, light alkenes and
aromatic hydrocarbons) at night, while it was strongly
influenced by local, biogenic emissions of isoprene during
the day. Box model calculations initialized by measured
parameters reproduce the observed OH reactivity well and
suggest that the missing reactivity is contributed by
unmeasured, secondary chemistry products (mainly aldehydes
and ketones) that were photochemically formed by hydrocarbon
oxidation. Overall, k(OH) was dominated by organic
compounds, which had a maximum contribution of $85\%$ in the
afternoon. The paper demonstrates the usefulness of direct
reactivity measurements, emphasizes the need for direct
measurements of oxygenated organic compounds in atmospheric
chemistry studies, and discusses uncertainties of the
modelling of OVOC reactivities.},
keywords = {J (WoSType)},
cin = {IEK-8 / JARA-HPC},
ddc = {550},
cid = {I:(DE-Juel1)IEK-8-20101013 / $I:(DE-82)080012_20140620$},
pnm = {Atmosphäre und Klima},
pid = {G:(DE-Juel1)FUEK491},
shelfmark = {Meteorology $\&$ Atmospheric Sciences},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000284759500029},
doi = {10.5194/acp-10-11243-2010},
url = {https://juser.fz-juelich.de/record/12502},
}