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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-5-2635-2005</article-id>
<title-group>
<article-title>Two decades of OH variability as inferred by an inversion of atmospheric transport and chemistry of methyl chloroform</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bousquet</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hauglustaine</surname>
<given-names>D. A.</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>Peylin</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Carouge</surname>
<given-names>C.</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>Ciais</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Laboratoire des Sciences du Climat et de l’Environnement (LSCE), Gif sur Yvette, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Université de Versailles Saint Quentin en Yvelines (UVSQ), Versailles, France</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Laboratoire de Biogéochimie des milieux continentaux, UMR INRA-CNRS-PARIS 6, INRA-INAPG, Thiverval-Grignon, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>04</day>
<month>10</month>
<year>2005</year>
</pub-date>
<volume>5</volume>
<issue>10</issue>
<fpage>2635</fpage>
<lpage>2656</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/5/2635/2005/acp-5-2635-2005.html">This article is available from http://www.atmos-chem-phys.net/5/2635/2005/acp-5-2635-2005.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/5/2635/2005/acp-5-2635-2005.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/5/2635/2005/acp-5-2635-2005.pdf</self-uri>
<abstract>
<p>We developed an iterative inverse method to infer inter-annual sources and
sinks of methyl chloroform (MCF) from atmospheric measurements, on a monthly
basis. The methodology is presented and used to estimate two decades of OH
variability between 1980 and 2000, using varying meteorology. When OH
concentrations are adjusted with loose prior errors and MCF emissions are
adjusted within inventory bounds, we show that substantial OH inter-annual
variability (8.5&amp;plusmn;1.0% of the mean) and trend
(-0.7%.yr&lt;sup&gt;-1&lt;/sup&gt;) are necessary to match MCF observations. This
result is confirmed by a series of sensitivity tests addressing main
limitations of previous studies. However, we show that it is also possible to
match MCF observations with a 65% reduction of OH year-to-year variations
and a 60% reduction of absolute OH trend, but still a consistency of
inferred emissions with inventory values at a &amp;plusmn;2&amp;sigma; level. On the
other hand, the phase of inferred OH variations is a more robust feature of
our set of inversions. Overall, MCF inversions can only provide a range of OH
variations unless inventory uncertainties are further reduced.</p>
</abstract>
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