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<front>
<journal-meta>
<journal-id journal-id-type="publisher">BG</journal-id>
<journal-title-group>
<journal-title>Biogeosciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">BG</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Biogeosciences</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1726-4189</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/bg-10-3767-2013</article-id>
<title-group>
<article-title>NW European shelf under climate warming: implications for open ocean &amp;ndash; shelf exchange, primary production, and carbon absorption</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gröger</surname>
<given-names>M.</given-names>
<ext-link>https://orcid.org/0000-0002-9927-5164</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Maier-Reimer</surname>
<given-names>E.</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>Mikolajewicz</surname>
<given-names>U.</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>Moll</surname>
<given-names>A.</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>Sein</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Max Planck Institute for Meteorology, Bundesstrasse 53, 20146  Hamburg, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institut für Meereskunde, Universität  Hamburg (CEN), Bundesstrasse 53, 20146 Hamburg, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>12</day>
<month>06</month>
<year>2013</year>
</pub-date>
<volume>10</volume>
<issue>6</issue>
<fpage>3767</fpage>
<lpage>3792</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 M. Gröger et al.</copyright-statement>
<copyright-year>2013</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/articles/10/3767/2013/bg-10-3767-2013.html">This article is available from https://bg.copernicus.org/articles/10/3767/2013/bg-10-3767-2013.html</self-uri>
<self-uri xlink:href="https://bg.copernicus.org/articles/10/3767/2013/bg-10-3767-2013.pdf">The full text article is available as a PDF file from https://bg.copernicus.org/articles/10/3767/2013/bg-10-3767-2013.pdf</self-uri>
<abstract>
<p>Shelves have been estimated to account for more than one-fifth of
  the global marine primary production.  It has been also conjectured
  that shelves strongly influence the oceanic absorption of
  anthropogenic CO&lt;sub&gt;2&lt;/sub&gt; (carbon shelf pump). Owing to their coarse
  resolution, currently applied global climate models are
  inappropriate to investigate the impact of climate change on shelves
  and regional models do not account for the complex interaction with
  the adjacent open ocean.  In this study, a global ocean general
  circulation model and biogeochemistry model were set up with
  a distorted grid providing a maximal resolution for the NW European
  shelf and the adjacent northeast Atlantic.
&lt;br&gt;&lt;br&gt;
  Using model climate projections we found that already a~moderate
  warming of about 2.0 K of the sea surface is linked with
  a reduction by ~ 30% of the biological production on the NW
  European shelf. If we consider the decline of anthropogenic riverine
  eutrophication since the 1990s, the reduction of biological production
  amounts is even larger. The relative decline of NW European shelf productivity
  is twice as strong as the decline in the open ocean
  (~ 15%).  The underlying mechanism is a spatially well
  confined stratification feedback along the continental shelf break.
  This feedback reduces the nutrient supply from the deep Atlantic to
  about 50%.  In turn, the reduced productivity draws down CO&lt;sub&gt;2&lt;/sub&gt; absorption in the North
Sea by ~ 34% at the end
  of the 21st century compared to the end of the 20th century implying
  a strong weakening of shelf carbon pumping. Sensitivity experiments
  with diagnostic tracers indicate that not more than 20% of the
  carbon absorbed in the North Sea contributes to the long-term carbon
  uptake of the world ocean. The rest remains within the ocean&apos;s mixed
  layer where it is exposed to the atmosphere.
&lt;br&gt;&lt;br&gt;
  The predicted decline in biological productivity, and decrease of
  phytoplankton concentration (in the North Sea by averaged 25%) due to reduced
  nutrient imports from the deeper Atlantic will probably
  affect the local fish stock negatively and therefore fisheries in the North
  Sea.</p>
</abstract>
<counts><page-count count="26"/></counts>
</article-meta>
</front>
<body/>
<back>
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