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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" specific-use="SMUR" dtd-version="3.0" xml:lang="en">
<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>
<abbrev-journal-title abbrev-type="nlm-ta">Biogeosciences Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1810-6285</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/bgd-11-2083-2014</article-id>
<title-group>
<article-title>Challenges and opportunities to reduce uncertainty in projections of future  atmospheric CO&lt;sub&gt;2&lt;/sub&gt;: a combined marine and terrestrial biosphere  perspective</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Dalmonech</surname>
<given-names>D.</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>Foley</surname>
<given-names>A. M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</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>Anav</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>Friedlingstein</surname>
<given-names>P.</given-names>
<ext-link>https://orcid.org/0000-0003-3309-4739</ext-link>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Friend</surname>
<given-names>A. D.</given-names>
<ext-link>https://orcid.org/0000-0002-9029-1045</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kidston</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>Willeit</surname>
<given-names>M.</given-names>
<ext-link>https://orcid.org/0000-0003-3998-6404</ext-link>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zaehle</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Biogeochemical Integration Department, Max Planck Institute    for Biogeochemistry, Hans-Knöll-Str. 10, 07745 Jena, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Geography, University of Cambridge, Downing Place,  Cambridge CB2 3EN, UK</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Cambridge Centre for Climate Change Mitigation Research, Department  of Land Economy, University of Cambridge, Cambridge, UK</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>College of Engineering, Mathematics and Physical Sciences,  University of Exeter, Exeter, EX4 4QF, UK</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Laboratoire des Sciences du Climat et l&apos;Environnement,  Gif-sur-Yvette, France</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Potsdam Institute for Climate Impact Research, Potsdam, Germany</addr-line>
</aff>
<funding-group>
<award-group id="gs1">
<funding-source>European Commission</funding-source>
<award-id>GREENCYCLESII - Anticipating climate change and biospheric feedbacks within the Earth system to 2200 (238366)</award-id>
</award-group>
</funding-group>
<pub-date pub-type="epub">
<day>04</day>
<month>02</month>
<year>2014</year>
</pub-date>
<volume>11</volume>
<issue>2</issue>
<fpage>2083</fpage>
<lpage>2153</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2014 D. Dalmonech et al.</copyright-statement>
<copyright-year>2014</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://bg.copernicus.org/preprints/11/2083/2014/bgd-11-2083-2014.html">This article is available from https://bg.copernicus.org/preprints/11/2083/2014/bgd-11-2083-2014.html</self-uri>
<self-uri xlink:href="https://bg.copernicus.org/preprints/11/2083/2014/bgd-11-2083-2014.pdf">The full text article is available as a PDF file from https://bg.copernicus.org/preprints/11/2083/2014/bgd-11-2083-2014.pdf</self-uri>
<abstract>
<p>Atmospheric CO&lt;sub&gt;2&lt;/sub&gt; and climate projections for the next century
  vary widely across current Earth system models (ESMs), owing to
  different representations of the interactions between the marine and
  land carbon cycle on the one hand, and climate change and increasing
  atmospheric CO&lt;sub&gt;2&lt;/sub&gt; on the other hand. Several efforts have been
  made in the last years to analyse these differences in detail in
  order to suggest model improvements. Here we review these efforts
  and analyse their successes, but also the associated uncertainties
  that hamper the best use of the available observations to constrain
  and improve the ESMs models. The aim of this paper is to highlight
  challenges in improving the ESMs that result from: (i) uncertainty
  about important processes in terrestrial and marine ecosystems and
  their response to climate change and increasing atmospheric
  CO&lt;sub&gt;2&lt;/sub&gt;; (ii) structural and parameter-related uncertainties in
  current land and marine models; (iii) uncertainties related to
  observations and the formulations of model performance metrics. We
  discuss the implications of these uncertainties for reducing the
  spread in future projections of ESMs and suggest future directions
  of work to overcome these uncertainties.</p>
</abstract>
<counts><page-count count="71"/></counts>
</article-meta>
</front>
<body/>
<back>
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