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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>8</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-12595-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/12595/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/12595/2008/acpd-8-12595-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/12595/2008/acpd-8-12595-2008.pdf</fulltext_pdf>
	<start_page>12595</start_page>
	<end_page>12624</end_page>
	<publication_date>2008-07-02</publication_date>
	<article_title content_type="html">The role of ice in N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; heterogeneous hydrolysis at high latitudes</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. L. Apodaca</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>D. M. Huff</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>W. R. Simpson</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Chemistry and Biochemistry and Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, 99775-6160, USA</affiliation>
	</affiliations>
	<abstract content_type="html">We report evidence for ice catalyzing N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; heterogeneous hydrolysis from a study
conducted near Fairbanks, AK in November 2007.  Mixing ratios of  N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;, NO, NO&lt;sub&gt;2&lt;/sub&gt;,
and ozone are reported and are used to determine steady state N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; lifetimes.  When air masses
are sub-saturated with respect to ice, the data show longer lifetimes (&amp;asymp;20 min) and elevated  N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; levels, while ice-saturated air masses show shorter lifetimes (&amp;asymp;6 min) and suppressed N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; levels.
We also report estimates of aerosol surface area densities that are on the order of 50 μm&lt;sup&gt;2&lt;/sup&gt;/cm&lt;sup&gt;3&lt;/sup&gt;, a surface area
density that is insufficient to explain the rapid losses of  N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; observed in this study, reinforcing the
importance of other reactive surfaces such as ice. Ice-saturated pollution plumes are ubiquitous in high
latitudes; therefore, catalysis on these surfaces is largely responsible for nocturnal processing of  N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;
leading to nitric acid production and loss of  NO&lt;sub&gt;x&lt;/sub&gt; in high latitude plumes.</abstract>
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</article>

