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<front>
<journal-meta>
<journal-id journal-id-type="publisher">BGD</journal-id>
<journal-title-group>
<journal-title>Biogeosciences Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">BGD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1810-6285</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/bgd-6-729-2009</article-id>
<title-group>
<article-title>Estimating the storage of anthropogenic carbon in the subtropical Indian  Ocean: a comparison of five different approaches</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Álvarez</surname>
<given-names>M.</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>Lo Monaco</surname>
<given-names>C.</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>Tanhua</surname>
<given-names>T.</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>Yool</surname>
<given-names>A.</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>Oschlies</surname>
<given-names>A.</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>Bullister</surname>
<given-names>J. L.</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>Goyet</surname>
<given-names>C.</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>Metzl</surname>
<given-names>N.</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>Touratier</surname>
<given-names>F.</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>McDonagh</surname>
<given-names>E.</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>Bryden</surname>
<given-names>H. L.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>IMEDEA (CSIC-UIB), Miquel Marqués 21, 07190 Esporles, Spain</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>LOCEAN/IPSL, Université Paris 6 – place Jussieu 4, 75252 Paris, France</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>IFM-GEOMAR, Düsternbrooker Weg 20, 24105 Kiel, Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>NOCS, Waterfront Campus European Way, Southampton, SO14 3ZH, UK</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>NOAA/Pacific Marine Environmental Laboratory, Seattle, Washington,  USA</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>IMAGES, Université de Perpignan, 52 avenue Paul Alduy, 66860  Perpignan, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>13</day>
<month>01</month>
<year>2009</year>
</pub-date>
<volume>6</volume>
<issue>1</issue>
<fpage>729</fpage>
<lpage>796</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.biogeosciences-discuss.net/6/729/2009/bgd-6-729-2009.html">This article is available from http://www.biogeosciences-discuss.net/6/729/2009/bgd-6-729-2009.html</self-uri>
<self-uri xlink:href="http://www.biogeosciences-discuss.net/6/729/2009/bgd-6-729-2009.pdf">The full text article is available as a PDF file from http://www.biogeosciences-discuss.net/6/729/2009/bgd-6-729-2009.pdf</self-uri>
<abstract>
<p>The subtropical Indian Ocean along 32&amp;deg; S was for the
      first time simultaneously sampled in 2002 for inorganic carbon and
      transient tracers. The vertical distribution and inventory of
      anthropogenic carbon (C&lt;sub&gt;ANT&lt;/sub&gt;) from five different methods: four
      data-base methods (ΔC*, TrOCA, TTD and C&lt;sup&gt;0&lt;/sup&gt;&lt;sub&gt;IPSL&lt;/sub&gt; and
      a simulation from the OCCAM model are compared and discussed along
      with the observed CFC-12 and CCl&lt;sub&gt;4&lt;/sub&gt; distributions. In the surface
      layer, where carbon-based methods are uncertain, TTD and OCCAM yield
      the same result (7&amp;plusmn;0.2 mol C m&lt;sup&gt;&amp;minus;2&lt;/sup&gt;), helping to specify
      the surface C&lt;sub&gt;ANT&lt;/sub&gt; inventory. Below the mixed-layer, the comparison
      suggests that C&lt;sub&gt;ANT&lt;/sub&gt; penetrates deeper and more uniformly into the
      Antarctic Intermediate Water layer limit than estimated from the
      &amp;Delta;C* method. Additionally, significant CFC-12 and
      CCl&lt;sub&gt;4&lt;/sub&gt; values are detected in bottom waters, associated with
      Antarctic Bottom Water. In this layer, except for &amp;Delta;C* and
      OCCAM, the other methods detect significant C&lt;sub&gt;ANT&lt;/sub&gt;
      values. Consequently, the lowest inventory is calculated using the
      ΔC* method (24&amp;plusmn;2 mol C m&lt;sup&gt;&amp;minus;2&lt;/sup&gt;) or OCCAM
      (24.4&amp;plusmn;2.8  mol C m&lt;sup&gt;&amp;minus;2&lt;/sup&gt;) while TrOCA, TTD, and
      C&lt;sup&gt;0&lt;/sup&gt;&lt;sub&gt;IPSL&lt;/sub&gt; lead to higher inventories (28.1&amp;plusmn;2.2, 28.9&amp;plusmn;2.3
      and 30.8&amp;plusmn;2.5 mol C m&lt;sup&gt;&amp;minus;2&lt;/sup&gt;, respectively). Overall and
      despite the uncertainties each method is evaluated using its
      relationship with tracers and the knowledge about water masses in the
      subtropical Indian Ocean. Along 32&amp;deg; S our best estimate
      for the mean C&lt;sub&gt;ANT&lt;/sub&gt; specific inventory is
      28&amp;plusmn;2 mol C m&lt;sup&gt;&amp;minus;2&lt;/sup&gt;. Comparison exercises for data-based
      C&lt;sub&gt;ANT&lt;/sub&gt; methods along with time-series or repeat sections analysis
      should help to identify strengths and caveats in the C&lt;sub&gt;ANT&lt;/sub&gt; methods
      and to better constrain model simulations.</p>
</abstract>
<counts><page-count count="68"/></counts>
</article-meta>
</front>
<body/>
<back>
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