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<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>8</volume_number>
		<issue_number>24</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acp-8-7451-2008</doi>
	<article_url>http://www.atmos-chem-phys.net/8/7451/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/8/7451/2008/acp-8-7451-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/8/7451/2008/acp-8-7451-2008.pdf</fulltext_pdf>
	<start_page>7451</start_page>
	<end_page>7463</end_page>
	<publication_date>2008-12-15</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, Alaska, 99 775-6160, 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, Alaska 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 &amp;mu;m&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.
Consideration of two possible responsible types of ice surfaces, the snowpack
and suspended ice particles, indicates that both are reasonable as possible
sinks for N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;. Because ice-saturated conditions are ubiquitous in
high latitudes, ice surfaces are likely to be a key loss 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>

