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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-5-563-2005</article-id>
<title-group>
<article-title>Increased Northern Hemispheric carbon monoxide burden in the troposphere in 2002 and 2003 detected from the ground and from space</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Yurganov</surname>
<given-names>L. N.</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>Duchatelet</surname>
<given-names>P.</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>Dzhola</surname>
<given-names>A. V.</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>Edwards</surname>
<given-names>D. P.</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>Hase</surname>
<given-names>F.</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>Kramer</surname>
<given-names>I.</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>Mahieu</surname>
<given-names>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>Mellqvist</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Notholt</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Novelli</surname>
<given-names>P. C.</given-names>
</name>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Rockmann</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Scheel</surname>
<given-names>H. E.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Schneider</surname>
<given-names>M.</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>Schulz</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff10">
<sup>10</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Strandberg</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sussmann</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tanimoto</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff11">
<sup>11</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Velazco</surname>
<given-names>V.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Drummond</surname>
<given-names>J. R.</given-names>
</name>
<xref ref-type="aff" rid="aff12">
<sup>12</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gille</surname>
<given-names>J. C.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Frontier Research Center for Global Change, JAMSTEC, Yokohama, Japan</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute of Astrophysics and Geophysics, University of Liège, Liège, Belgium</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Obukhov Institute of Atmospheric Physics, Moscow, Russia</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Atmospheric Chemistry Division, National Center for Atmospheric Research, Boulder, CO, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>IMK-ASF, Forschungszentrum Karlsruhe, Karlsruhe, Germany</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Radio and Space Science, Chalmers University of Technology, Göteborg, Sweden</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>University of Bremen, Bremen, Germany</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>Climate Monitoring and Diagnostic Laboratory, NOAA, Boulder, Colorado, USA</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>IMK-IFU, Forschungszentrum Karlsruhe, Garmisch-Partenkirchen, Germany</addr-line>
</aff>
<aff id="aff10">
<label>10</label>
<addr-line>Alfred-Wegener-Institute, Potsdam, Germany</addr-line>
</aff>
<aff id="aff11">
<label>11</label>
<addr-line>National Institute for Environmental Studies, Tsukuba, Japan</addr-line>
</aff>
<aff id="aff12">
<label>12</label>
<addr-line>University of Toronto, Toronto, Canadar</addr-line>
</aff>
<pub-date pub-type="epub">
<day>21</day>
<month>02</month>
<year>2005</year>
</pub-date>
<volume>5</volume>
<issue>2</issue>
<fpage>563</fpage>
<lpage>573</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/5/563/2005/acp-5-563-2005.html">This article is available from http://www.atmos-chem-phys.net/5/563/2005/acp-5-563-2005.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/5/563/2005/acp-5-563-2005.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/5/563/2005/acp-5-563-2005.pdf</self-uri>
<abstract>
<p>Carbon monoxide total column amounts in the atmosphere
have been measured in the High Northern Hemisphere (30&amp;deg;-90&amp;deg; N,
HNH) between January 2002 and December 2003 using infrared spectrometers of
high and moderate resolution and the Sun as a light source. They were
compared to ground-level CO mixing ratios and to total column amounts
measured from space by the Terra/MOPITT instrument. All these data reveal
increased CO abundances in 2002-2003 in comparison to the unperturbed
2000-2001 period. Maximum anomalies were observed in September 2002 and
August 2003. Using a simple two-box model, the corresponding annual CO
emission anomalies (referenced to 2000-2001 period) have been found equal to
95Tg in 2002 and 130Tg in 2003, thus close to those for 1996 and 1998. A
good correlation with hot spots detected by a satellite radiometer allows
one to assume strong boreal forest fires, occurred mainly in Russia, as a
source of the increased CO burdens.</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
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<back>
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</article>