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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-8-5731-2008</article-id>
<title-group>
<article-title>Odin stratospheric proxy NO&lt;sub&gt;y&lt;/sub&gt; measurements and climatology</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Brohede</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>McLinden</surname>
<given-names>C. A.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Urban</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Haley</surname>
<given-names>C. S.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jonsson</surname>
<given-names>A. I.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Murtagh</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Radio and Space Science, Chalmers University of Technology, 412 96 GÃ¶teborg, Sweden</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Environment Canada, 4905 Dufferin Street, Toronto, Ontario, M3H 5T4, Canada</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Centre for Research in Earth and Space Science, York University, 4700 Keele Street, Toronto, Ontario, M3J 1P3, Canada</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Physics, University of Toronto, M5S 1A7 Toronto, Ontario, Canada</addr-line>
</aff>
<pub-date pub-type="epub">
<day>01</day>
<month>10</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>19</issue>
<fpage>5731</fpage>
<lpage>5754</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys.net/8/5731/2008/acp-8-5731-2008.html">This article is available from http://www.atmos-chem-phys.net/8/5731/2008/acp-8-5731-2008.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/8/5731/2008/acp-8-5731-2008.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/8/5731/2008/acp-8-5731-2008.pdf</self-uri>
<abstract>
<p>Five years of OSIRIS (Optical Spectrograph and InfraRed Imager System) NO&lt;sub&gt;2&lt;/sub&gt;
and SMR (Sub-millimetre and Millimetre Radiometer) HNO&lt;sub&gt;3&lt;/sub&gt; observations from
the Odin satellite, combined with data from a photochemical box model, have
been used to construct a stratospheric proxy NO&lt;sub&gt;y&lt;/sub&gt; data set including the
gases: NO, NO&lt;sub&gt;2&lt;/sub&gt;, HNO&lt;sub&gt;3&lt;/sub&gt;, 2&amp;times;N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; 
and ClONO&lt;sub&gt;2&lt;/sub&gt;. This Odin NO&lt;sub&gt;y&lt;/sub&gt; 
climatology is based on all daytime measurements and contains monthly mean
and standard deviation, expressed as mixing ratio or number density, as
function of latitude or equivalent latitude (5&amp;deg; bins) on 17 vertical
layers (altitude, pressure or potential temperature) between 14 and 46 km.
Comparisons with coincident NO&lt;sub&gt;y&lt;/sub&gt; profiles from the Atmospheric Chemistry
Experiment-Fourier Transform Spectrometer (ACE-FTS) instrument were used to
evaluate several methods to combine Odin observations with model data. This
comparison indicates that the most appropriate merging technique uses OSIRIS
measurements of NO&lt;sub&gt;2&lt;/sub&gt;, scaled with model NO/NO&lt;sub&gt;2&lt;/sub&gt; ratios, to estimate NO.
The sum of 2&amp;times;N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; and ClONO&lt;sub&gt;2&lt;/sub&gt; is estimated from
uncertainty-based weighted averages of scaled observations of SMR HNO&lt;sub&gt;3&lt;/sub&gt; and
OSIRIS NO&lt;sub&gt;2&lt;/sub&gt;. Comparisons with ACE-FTS suggest the precision (random error)
and accuracy (systematic error) of Odin NO&lt;sub&gt;y&lt;/sub&gt; profiles are about 15% and
20%, respectively. Further comparisons between Odin and the Canadian Middle
Atmosphere Model (CMAM) show agreement to within 20% and 2 ppb throughout
most of the stratosphere except in the polar vortices. The combination of
good temporal and spatial coverage, a relatively long data record, and good
accuracy and precision make this a valuable NO&lt;sub&gt;y&lt;/sub&gt; product for various
atmospheric studies and model assessments.</p>
</abstract>
<counts><page-count count="24"/></counts>
</article-meta>
</front>
<body/>
<back>
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