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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>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-11-10743-2011</article-id>
<title-group>
<article-title>TES ammonia retrieval strategy and global observations of the spatial and seasonal variability of ammonia</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Shephard</surname>
<given-names>M. W.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cady-Pereira</surname>
<given-names>K. E.</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>Luo</surname>
<given-names>M.</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>Henze</surname>
<given-names>D. K.</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>Pinder</surname>
<given-names>R. W.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Walker</surname>
<given-names>J. T.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Rinsland</surname>
<given-names>C. P.</given-names>
</name>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bash</surname>
<given-names>J. O.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhu</surname>
<given-names>L.</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>Payne</surname>
<given-names>V. H.</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>Clarisse</surname>
<given-names>L.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Environment Canada, Downsview, Ontario, Canada</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Atmospheric and Environmental Research, Inc., Lexington, Massachusetts, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Jet Propulsion Laboratory, California Institute of Technology Pasadena, CA, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>University of Colorado, Boulder, Colorado, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>US Environmental Protection Agency, Research Triangle Park, North Carolina, USA</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Spectroscopie de l&apos;Atmosphere, Service de Chimie Quantique et Photophysique, Universite Libre de Bruxelles (U.L.B.), Brussels, Belguim</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>presently at: Atmospheric and Climate Applications (ACApps), Inc., East Gwillimbury, Ontario, Canada</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>formerly at: NASA Langley Research Center, Hampton, VA, USA</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>deceased</addr-line>
</aff>
<pub-date pub-type="epub">
<day>31</day>
<month>10</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>20</issue>
<fpage>10743</fpage>
<lpage>10763</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/11/10743/2011/acp-11-10743-2011.html">This article is available from http://www.atmos-chem-phys.net/11/10743/2011/acp-11-10743-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/10743/2011/acp-11-10743-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/10743/2011/acp-11-10743-2011.pdf</self-uri>
<abstract>
<p>Presently only limited sets of tropospheric ammonia
(NH&lt;sub&gt;3&lt;/sub&gt;) measurements in the Earth&apos;s atmosphere have been reported from
satellite and surface station measurements, despite the well-documented
negative impact of NH&lt;sub&gt;3&lt;/sub&gt; on the environment and human health. Presented
here is a detailed description of the satellite retrieval strategy and
analysis for the Tropospheric Emission Spectrometer (TES) using simulations
and measurements. These results show that: (i) the level of detectability
for a representative boundary layer TES NH&lt;sub&gt;3&lt;/sub&gt; mixing ratio value is ~0.4 ppbv, which typically corresponds to a profile that contains a maximum
level value of ~1 ppbv; (ii) TES NH&lt;sub&gt;3&lt;/sub&gt; retrievals generally provide at most
one degree of freedom for signal (DOFS), with peak sensitivity between 700
and 900 mbar; (iii) TES NH&lt;sub&gt;3&lt;/sub&gt; retrievals show significant spatial and
seasonal variability of NH&lt;sub&gt;3&lt;/sub&gt; globally; (iv) initial comparisons of TES
observations with GEOS-CHEM estimates show TES values being higher overall.
Important differences and similarities between modeled and observed seasonal
and spatial trends are noted, with discrepancies indicating areas where the
timing and magnitude of modeled NH&lt;sub&gt;3&lt;/sub&gt; emissions from agricultural
sources, and to lesser extent biomass burning sources, need further study.</p>
</abstract>
<counts><page-count count="21"/></counts>
</article-meta>
</front>
<body/>
<back>
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