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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys.net/inc/acp/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>5</volume_number>
		<issue_number>12</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acp-5-3441-2005</doi>
	<article_url>http://www.atmos-chem-phys.net/5/3441/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/5/3441/2005/acp-5-3441-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/5/3441/2005/acp-5-3441-2005.pdf</fulltext_pdf>
	<start_page>3441</start_page>
	<end_page>3450</end_page>
	<publication_date>2005-12-20</publication_date>
	<article_title content_type="html">On the changing seasonal cycles and trends of ozone at Mace Head, Ireland</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. C. Carslaw</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute for Transport Studies, University of Leeds, Leeds LS2 9JT, UK</affiliation>
	</affiliations>
	<abstract content_type="html">A seasonal-trend decomposition technique based on a locally-weighted
regression smoothing (Loess) approach has been used to decompose monthly
ozone concentrations at Mace Head (Ireland) into trend, seasonal and
irregular components. The trend component shows a steady increase from
1990&amp;ndash;2004, which is confirmed by statistical testing which shows that ozone
concentrations at Mace Head have increased at the p=0.06 level by
0.18&amp;plusmn;0.04 ppb yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt;. By considering different air mass origins using
a trajectory analysis, it has been possible to separate air masses into
&quot;polluted&quot; and &quot;unpolluted&quot; origins. The seasonal-trend decomposition
technique confirms the different seasonal cycles of these air mass origins
with unpolluted air mass maxima in April and polluted air mass maxima in
July/August. A detailed consideration of the seasonal component reveals
different behaviour depending on the air mass origin. For baseline
unpolluted air arriving at Mace Head there has been a gradual increase in
the seasonal amplitude, driven by a declining summertime component. The
amplitude of the seasonal component of baseline air is controlled by a
maximum in April and a minimum in July. For polluted air mass trajectories,
there was a substantial reduction in the amplitude of the seasonal component
from 1990&amp;ndash;1997. However, post-1997 results indicate that the seasonal
amplitude in polluted air masses arriving at Mace Head is increasing.
Furthermore, there has been a shift in the months controlling the size of
the seasonal amplitude in polluted air from a maximum in May and minimum in
January in 1990 to a maximum in April and a minimum in July by 2001. This
finding suggests that there has been a steadily decreasing influence of
polluted air masses arriving from Europe. These air masses have therefore
increasingly taken on the attributes of baseline air.</abstract>
	<references>
	</references>
</article>

