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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>4</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/acpd-4-6645-2004</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/4/6645/2004/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/4/6645/2004/acpd-4-6645-2004.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/4/6645/2004/acpd-4-6645-2004.pdf</fulltext_pdf>
	<start_page>6645</start_page>
	<end_page>6665</end_page>
	<publication_date>2004-10-15</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>
			<email>cohen@cchem.berkeley.edu</email>
		</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 200 pmol/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 30 min. 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 14 h 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>

