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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<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>5</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-5957-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/5957/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/5957/2005/acpd-5-5957-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/5957/2005/acpd-5-5957-2005.pdf</fulltext_pdf>
	<start_page>5957</start_page>
	<end_page>5985</end_page>
	<publication_date>2005-08-15</publication_date>
	<article_title content_type="html">Can we explain the trends in European ozone levels?</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. E. Jonson</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>D. Simpson</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>H. Fagerli</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>S. Solberg</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Norwegian Meteorological Institute, Oslo, Norway</affiliation>
		<affiliation numeration="2" content_type="html">Norwegian Institute for Air Research (NILU), Kjeller, Norway</affiliation>
	</affiliations>
	<abstract content_type="html">Ozone levels in Europe are changing.
Emissions of ozone precursors from Europe (NO&lt;sub&gt;x&lt;/sub&gt;, CO and non-methane
hydrocarbons) have been substantially reduced over
the last 10&amp;ndash;15 years, but changes in ozone levels can not be explained by
changes in European emissions alone.

&lt;br&gt;&lt;br&gt;
In order to explain the European trends in ozone since 1990
the EMEP regional photochemistry model has been run for the the years
1990 and 1995&amp;ndash;2002. The EMEP model is a regional model centered over Europe
but the model domain also includes most of the North Atlantic and the polar
region. Climatological ozone data are used as initial and lateral
boundary concentrations. Model results are compared to measurements over
this timespan of 12 years. Possible causes for the measured trends in
European surface ozone have been investigated using  model
sensitivity runs perturbing emissions and lateral boundary concentrations.
The observed ozone trends at many European sites are only partially
reproduced by global or regional photochemistry models, and possible
reasons for this are discussed. The increase in winter ozone partially
and the decrease in the magnitude of high ozone episodes is attributed to
the decrease in ozone precursor emissions since 1990 by the model.
Furthermore, the model calculations indicate that the emission reductions
has resulted in a marked decrease in summer ozone in major parts of Europe,
and in particular in Germany. Such a trend in summer ozone is likely to be
difficult to identify from the measurements because of large inter-annual
variability.</abstract>
	<references>
	</references>
</article>

