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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>9</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-11185-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/11185/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/11185/2009/acpd-9-11185-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/11185/2009/acpd-9-11185-2009.pdf</fulltext_pdf>
	<start_page>11185</start_page>
	<end_page>11220</end_page>
	<publication_date>2009-05-05</publication_date>
	<article_title content_type="html">Quantifying atmospheric nitrate formation pathways based on a global model of the oxygen  isotopic composition (&amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O) of atmospheric nitrate</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>B. Alexander</name>
			<email>beckya@u.washington.edu</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>M. G. Hastings</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>D. J. Allman</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>J. Dachs</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>J. A. Thornton</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>S. A. Kunasek</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA</affiliation>
		<affiliation numeration="2" content_type="html">Department of Geological Sciences and Environmental Change Initiative, Brown University, Providence, RI, USA</affiliation>
		<affiliation numeration="3" content_type="html">Department of Environmental Chemistry, Instituto de Investigaciones Químicas y Ambientales  de Barcelona/Consejo Superior de Investigaciones Científicas, Barcelona, Spain</affiliation>
		<affiliation numeration="4" content_type="html">Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The oxygen isotopic composition (&amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O) of atmospheric nitrate is a function
      of the relative abundance of atmospheric oxidants (O&lt;sub&gt;3&lt;/sub&gt;, HO&lt;sub&gt;x&lt;/sub&gt;=OH
      +HO&lt;sub&gt;2&lt;/sub&gt;+RO&lt;sub&gt;2&lt;/sub&gt;) and the formation pathway of nitrate from its precursor
      NO&lt;sub&gt;x&lt;/sub&gt; (=NO+NO&lt;sub&gt;2&lt;/sub&gt;). Coupled observations and modeling of nitrate
      &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O can be used to quantify the relative importance of chemical formation
      pathways leading to nitrate formation and reduce uncertainties in the budget of reactive
      nitrogen chemistry in the atmosphere. We present the first global model of atmospheric
      nitrate &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O and compare with available observations. The model shows the
      best agreement with a global compilation of observations when assuming
      a &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O value of tropospheric ozone equal to 35&amp;permil; and preferential
      oxidation of NO&lt;sub&gt;x&lt;/sub&gt; by the terminal oxygen atoms of ozone. Calculated values of
      annual-mean nitrate &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O in the lowest model layer (0–200 m above
      the surface) vary from 6&amp;permil; in the tropics to 41&amp;permil; in the polar-regions. On the
      global scale, O&lt;sub&gt;3&lt;/sub&gt; is the dominant oxidant (81% annual-mean) during NO&lt;sub&gt;x&lt;/sub&gt;
      cycling reactions. The global, annual-mean tropospheric inorganic nitrate burden is
      dominated by nitrate formation via NO&lt;sub&gt;2&lt;/sub&gt;+OH (76%), followed by
      N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; hydrolysis (18%) and NO&lt;sub&gt;3&lt;/sub&gt;+DMS/HC
      (4%). Model discrepancies are largest in the polar spring and summer, most likely due to
      the lack of reactive halogen chemistry in the model. The influence of organic nitrates on
      observations of nitrate &amp;Delta;&lt;sup&gt;17&lt;/sup&gt;O needs to be determined, especially for
      observations in summertime and tropical forested regions where organic nitrates can
      contribute up to 80% of the total NO&lt;sub&gt;y&lt;/sub&gt; (organic plus inorganic nitrate) budget.</abstract>
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</article>

