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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>6</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acpd-6-11427-2006</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/6/11427/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/6/11427/2006/acpd-6-11427-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/6/11427/2006/acpd-6-11427-2006.pdf</fulltext_pdf>
	<start_page>11427</start_page>
	<end_page>11464</end_page>
	<publication_date>2006-11-16</publication_date>
	<article_title content_type="html">The weekend effect within and downwind of Sacramento: Part 1. Observations of ozone, nitrogen oxides, and VOC reactivity</article_title>
	<authors>
		<author numeration="1" affiliations="1,4">
			<name>J. G. Murphy</name>
		</author>
		<author numeration="2" affiliations="1,5">
			<name>D. A. Day</name>
		</author>
		<author numeration="3" affiliations="1,6">
			<name>P. A. Cleary</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>P. J. Wooldridge</name>
		</author>
		<author numeration="5" affiliations="2,7">
			<name>D. B. Millet</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>A. H. Goldstein</name>
		</author>
		<author numeration="7" affiliations="1,3">
			<name>R. C. Cohen</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">University of California at Berkeley, Department of Chemistry, Berkeley, CA, USA</affiliation>
		<affiliation numeration="2" content_type="html">University of California at Berkeley, Department of Environmental Science, Policy and Management, Berkeley, CA, USA</affiliation>
		<affiliation numeration="3" content_type="html">University of California at Berkeley, Department of Earth and Planetary Sciences, Berkeley, CA, USA</affiliation>
		<affiliation numeration="4" content_type="html">now at: University of East Anglia, School of Environmental Sciences, Norwich, UK</affiliation>
		<affiliation numeration="5" content_type="html">now at: University of California at Davis, Land, Air and Water Resources Department, Davis, CA, USA</affiliation>
		<affiliation numeration="6" content_type="html">now at: University of Pennsylvania, Department of Chemistry, Philadelphia, PA, USA</affiliation>
		<affiliation numeration="7" content_type="html">now at: Harvard University, Department of Earth and Planetary Sciences, Cambridge, MA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Day-of-week patterns in human activities can be used to examine the ways in
which differences in primary emissions result in changes in the rates of
photochemical reactions, and the production of secondary pollutants. Data
from twelve California Air Resources Board monitoring sites in Sacramento,
CA, and the downwind Mountain Counties air basin are analyzed to reveal day
of week patterns in ozone and its precursors in the summers of 1998&amp;ndash;2002.
This routine monitoring data is complemented by comprehensive data sets of
ozone and nitrogen oxide concentrations and VOC reactivity obtained in the
summers of 2001 and 2003 at three sites in the region. Daytime
concentrations of nitrogen oxides (NO&lt;sub&gt;x&lt;/sub&gt;) are approximately 35% lower
on weekends at all the sites, whereas the VOC reactivity changes by less
than 10%. All six sites in the Sacramento Valley have higher 8-h
maximum average ozone on the weekend and are more likely to exceed the
national standard of 85 ppb on the weekend. In contrast, all the sites in
the Mountain Counties are less likely to exceed the federal ozone standard
on the weekend. Analysis of the day-of-week trends in odd oxygen show that
the weekend effect of ozone within Sacramento is strongly influenced by NO
sources close to the monitoring sites. This suggests that ozone measurements
from monitoring sites close to highways, including two rural locations, may
not be representative of the regional abundance, and lead to underestimates
of long term exposure for humans and ecosystems.</abstract>
	<references>
	</references>
</article>

