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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>2</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acp-5-483-2005</doi>
	<article_url>http://www.atmos-chem-phys.net/5/483/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/5/483/2005/acp-5-483-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/5/483/2005/acp-5-483-2005.pdf</fulltext_pdf>
	<start_page>483</start_page>
	<end_page>491</end_page>
	<publication_date>2005-02-15</publication_date>
	<article_title content_type="html">Measurements of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;, NO&lt;sub&gt;2&lt;/sub&gt;, and O&lt;sub&gt;3&lt;/sub&gt; east of the San Francisco Bay</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>E. C. Wood</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>T. H. Bertram</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>P. J. Wooldridge</name>
		</author>
		<author numeration="4" affiliations="1,2,3">
			<name>R. C. Cohen</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Chemistry, University of California, Berkeley, California</affiliation>
		<affiliation numeration="2" content_type="html">Department of Earth and Planetary Sciences, University of California, Berkeley, California</affiliation>
		<affiliation numeration="3" content_type="html">Energy and Environment Technologies Division, Lawrence Berkeley National Laboratory, Berkeley, California</affiliation>
	</affiliations>
	<abstract content_type="html">We report in situ measurements of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;, NO&lt;sub&gt;2&lt;/sub&gt;, and O&lt;sub&gt;3&lt;/sub&gt; in
Contra Costa County, California during January 2004. Mixing ratios of
N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;, an intermediate compound in the atmosphere&apos;s nocturnal
cleansing process, ranged up to 200pmol/mol at night. The highest
N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; concentrations were correlated with low O&lt;sub&gt;3&lt;/sub&gt; and high
NO&lt;sub&gt;2&lt;/sub&gt; concentrations. The calculated steady state lifetime for
N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; ranged from 5 to 30min. The total HNO&lt;sub&gt;3&lt;/sub&gt; produced by
N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; hydrolysis over a 14h night was comparable to ambient
NO&lt;sub&gt;2&lt;/sub&gt; concentrations, and is estimated to be a factor of nine bigger than
the HNO&lt;sub&gt;3&lt;/sub&gt; produced during the day.</abstract>
	<references>
	</references>
</article>

