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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>8</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-18219-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/18219/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/18219/2008/acpd-8-18219-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/18219/2008/acpd-8-18219-2008.pdf</fulltext_pdf>
	<start_page>18219</start_page>
	<end_page>18266</end_page>
	<publication_date>2008-10-21</publication_date>
	<article_title content_type="html">The impact of traffic emissions on atmospheric ozone and OH: results from QUANTIFY</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. Hoor</name>
			<email>hoor@mpch-mainz.mpg.de</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>J. Borken-Kleefeld</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>D. Caro</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>O. Dessens</name>
		</author>
		<author numeration="5" affiliations="5">
			<name>O. Endresen</name>
		</author>
		<author numeration="6" affiliations="6">
			<name>M. Gauss</name>
		</author>
		<author numeration="7" affiliations="7">
			<name>V. Grewe</name>
		</author>
		<author numeration="8" affiliations="3">
			<name>D. Hauglustaine</name>
		</author>
		<author numeration="9" affiliations="6">
			<name>I. S. A. Isaksen</name>
		</author>
		<author numeration="10" affiliations="1">
			<name>P. JÃ¶ckel</name>
		</author>
		<author numeration="11" affiliations="1">
			<name>J. Lelieveld</name>
		</author>
		<author numeration="12" affiliations="8">
			<name>E. Meijer</name>
		</author>
		<author numeration="13" affiliations="9">
			<name>D. Olivie</name>
		</author>
		<author numeration="14" affiliations="10">
			<name>M. Prather</name>
		</author>
		<author numeration="15" affiliations="11">
			<name>C. Schnadt Poberaj</name>
		</author>
		<author numeration="16" affiliations="11">
			<name>J. Staehelin</name>
		</author>
		<author numeration="17" affiliations="10">
			<name>Q. Tang</name>
		</author>
		<author numeration="18" affiliations="12">
			<name>J. van Aardenne</name>
		</author>
		<author numeration="19" affiliations="8">
			<name>P. van Velthoven</name>
		</author>
		<author numeration="20" affiliations="7">
			<name>R. Sausen</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Max Planck Institute for Chemistry, Department of Atmospheric Chemistry, 55020 Mainz, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Transportation Studies, German Aerospace Center (DLR), Berlin, Germany</affiliation>
		<affiliation numeration="3" content_type="html">Laboratoire des Sciences du Climat et de l&apos;Environment (LSCE), CEN de Saclay, Gif-sur-Yvette, France</affiliation>
		<affiliation numeration="4" content_type="html">Centre for Atmospheric Science, Department of Chemistry, Cambridge, UK</affiliation>
		<affiliation numeration="5" content_type="html">DNV, Det Norske Veritas (DNV), Oslo, Norway</affiliation>
		<affiliation numeration="6" content_type="html">Department of Geosciences, University of Oslo, Norway</affiliation>
		<affiliation numeration="7" content_type="html">Deutsches Zentrum fÃ¼r Luft- und Raumfahrt, Institut fÃ¼r Physik der AtmosphÃ¤re, Oberpaffenhofen, 82234 Wessling, Germany</affiliation>
		<affiliation numeration="8" content_type="html">Royal Netherlands Meteorological Institute, KNMI, De Bilt, The Netherlands</affiliation>
		<affiliation numeration="9" content_type="html">Meteo France, CNRS, Toulouse, France</affiliation>
		<affiliation numeration="10" content_type="html">Department of Earth System Science, University of California, Irvine, USA</affiliation>
		<affiliation numeration="11" content_type="html">Institute for Atmospheric and Climate Science, Swiss Federal Institute of Technology, ZÃ¼rich, Switzerland</affiliation>
		<affiliation numeration="12" content_type="html">Joint Research Center, JRC, Ispra, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">To estimate the impact of emissions by road, aircraft and ship traffic on
ozone and OH of the present-day atmosphere seven different atmospheric chemistry
models simulated the atmospheric composition of the year 2003.
Based on newly developed global emission inventories for road, maritime and
aircraft emission data sets each model performed a series of five simulations: A
base scenario using the full set of emissions, three sensitivity studies with
each individual sector of transport reduced by 5% and one simulation with all
traffic related emissions reduced by 5%. The approach minimizes non-linearities
in atmospheric chemical effects and are later scaled to 100%.
&lt;br&gt;&lt;br&gt;
The global annual mean impact of ship emissions on ozone in the boundary layer
leads to an increase of ozone of 1.2%, followed by road (0.87%) and
aircraft emissions (0.3%). In the upper
troposphere between 200â€“300 hPa both road and ship traffic affect ozone by 1.1%, whereas
aircraft emissions contribute 0.9%. However, the
sensitivity of ozone formation per NO&lt;sub&gt;x&lt;/sub&gt; molecule emitted is highest for aircraft exhausts.
&lt;br&gt;&lt;br&gt;
The local maximum effect of the summed traffic emissions on
the ozone column predicted by the models is 4.0 DU and occurs over the northern
subtropical Atlantic. The impact of traffic emissions on total ozone in the
Southern Hemisphere is approximately half of the northern hemispheric perturbation.
&lt;br&gt;&lt;br&gt;
Below 800 hPa both ozone and OH
respond most sensitively to ship emissions in the marine boundary layer
over the Atlantic, where the effect can exceed 10% (zonal mean) which is 80%
of the total traffic induced ozone perturbation.
In the Southern Hemisphere ship
emissions contribute relatively strongly to the total ozone perturbation by
60%â€“80% throughout the year (equivalent to 1â€“1.5 ppbv).
&lt;br&gt;&lt;br&gt;
Road emissions have the strongest impact on ozone in the continental boundary
layer and the free troposphere in summer. They also affect the upper
troposphere particularly during northern summer associated with strong
convection in mid latitudes.
Ozone perturbations due to road traffic show the strongest seasonal cycle
in the northern troposphere, and can even change sign in the continental
boundary layer during winter.
&lt;br&gt;&lt;br&gt;
The OH concentration in the boundary layer is most strongly affected by ship
emissions, which has a significant influence on the lifetime of many trace
gases including methane. Methane lifetime changes due to ship emissions amount
to 4.1%, followed by road (1.6%) and air traffic (1.0%).</abstract>
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</article>

