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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>I. Colin Prentice</dc:contributor>
  <dc:contributor>Sarah Cornell</dc:contributor>
  <dc:contributor>T Davies-Barnard</dc:contributor>
  <dc:contributor>Adrien Finzi</dc:contributor>
  <dc:contributor>Oskar Franklin</dc:contributor>
  <dc:contributor>Ivan Janssens</dc:contributor>
  <dc:contributor>Tuula Larmola</dc:contributor>
  <dc:contributor>Stefano Manzoni</dc:contributor>
  <dc:contributor>Torgny Nasholm</dc:contributor>
  <dc:contributor>John Raven</dc:contributor>
  <dc:contributor>Karin Rebel</dc:contributor>
  <dc:contributor>Sasha C. Reed</dc:contributor>
  <dc:contributor>Sara Vicca</dc:contributor>
  <dc:contributor>Andy Wiltshire</dc:contributor>
  <dc:contributor>Sonke Zaehle</dc:contributor>
  <dc:creator>Benjamin Stocker</dc:creator>
  <dc:date>2016</dc:date>
  <dc:description>&lt;div class="t m0 x0 h4 y6 ff4 fs3 fc1 sc0 ls0 ws0"&gt;Understanding the degree to which nitrogen (N) availability limits land carbon (C) uptake under global environmental change represents an unresolved challenge. First-generation &amp;lsquo;C-only&amp;rsquo;vegetation models, lacking explicit representations of N cycling,projected a substantial and increasing land C sink under rising atmospheric CO&lt;sub&gt;2&lt;/sub&gt; concentrations. This prediction was questioned for not taking into account the potentially limiting effect of N availability, which is necessary for plant growth (Hungate et al.,2003). More recent global models include coupled C and N cycles in land ecosystems (C&amp;ndash;N models) and are widely assumed to be more realistic. However, inclusion of more processes has not consistently improved their performance in capturing observed responses of the global C cycle (e.g. Wenzel et al., 2014). With the advent of a new generation of global models, including coupled C, N, and phosphorus (P) cycling, model complexity is sure to increase; but model reliability may not, unless greater attention is paid to the correspondence of model process representations ande mpirical evidence. It was in this context that the &amp;lsquo;Nitrogen Cycle Workshop&amp;rsquo; at Dartington Hall, Devon, UK was held on 1&amp;ndash;5 February 2016. Organized by I. Colin Prentice and Benjamin D. Stocker (Imperial College London, UK), the workshop was funded by the European Research Council,project &amp;lsquo;Earth system Model Bias Reduction and assessing Abrupt Climate change&amp;rsquo; (EMBRACE). We gathered empirical ecologists and ecosystem modellers to identify key uncertainties in terrestrial C&amp;ndash;N cycling, and to discuss processes that are missing or poorly represented in current models.&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1111/nph.13997</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Blackwell Science</dc:publisher>
  <dc:title>Terrestrial nitrogen cycling in Earth system models revisited</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>