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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</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/acpd-3-5977-2003</article-id>
<title-group>
<article-title>Technical note: an interannual inversion method for continuous CO&lt;sub&gt;2&lt;/sub&gt; data</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Law</surname>
<given-names>R. M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>CSIRO Atmospheric Research, Aspendale, Victoria, Australia</addr-line>
</aff>
<pub-date pub-type="epub">
<day>21</day>
<month>11</month>
<year>2003</year>
</pub-date>
<volume>3</volume>
<issue>6</issue>
<fpage>5977</fpage>
<lpage>6000</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>
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<abstract>
<p>A sequential synthesis inversion method is described to estimate
      CO&lt;sub&gt;2&lt;/sub&gt; sources from continuous atmospheric data.  The sequential method makes
      the problem computationally feasible.  The method is assessed using four-hourly
      synthetic concentration data generated from known sources.  Multi-year mean sources and seasonal cycles are estimated with comparable quality as
      those from a traditional inversion of monthly mean data. Interannual variations in the estimated sources
      are closer to those of the known sources using the four-hourly data rather than
      monthly data.  The computational cost of the basis function simulations can be reduced by generating responses
      that are only six months long.  This does not significantly degrade the inversion results compared to using responses that are 12 months
      in length.</p>
</abstract>
<counts><page-count count="24"/></counts>
</article-meta>
</front>
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