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<front>
<journal-meta>
<journal-id journal-id-type="publisher">CP</journal-id>
<journal-title-group>
<journal-title>Climate of the Past</journal-title>
<abbrev-journal-title abbrev-type="publisher">CP</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Clim. Past</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1814-9332</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/cp-10-887-2014</article-id>
<title-group>
<article-title>Temperature reconstruction from 10 to 120 kyr b2k from the NGRIP ice core</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kindler</surname>
<given-names>P.</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>Guillevic</surname>
<given-names>M.</given-names>
<ext-link>https://orcid.org/0000-0002-8128-7247</ext-link>
</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>Baumgartner</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>Schwander</surname>
<given-names>J.</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>Landais</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>Leuenberger</surname>
<given-names>M.</given-names>
<ext-link>https://orcid.org/0000-0003-4299-6793</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Climate and Environmental Physics, Physics Institute and Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institut Pierre-Simon Laplace/Laboratoire des Sciences du Climat et de l&apos;Environnement, Gif-sur-Yvette, France</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Centre for Ice and Climate, Niels Bohr Institute, Universtity of Copenhagen, Copenhagen, Denmark</addr-line>
</aff>
<pub-date pub-type="epub">
<day>30</day>
<month>04</month>
<year>2014</year>
</pub-date>
<volume>10</volume>
<issue>2</issue>
<fpage>887</fpage>
<lpage>902</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2014 P. Kindler 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://cp.copernicus.org/articles/10/887/2014/cp-10-887-2014.html">This article is available from https://cp.copernicus.org/articles/10/887/2014/cp-10-887-2014.html</self-uri>
<self-uri xlink:href="https://cp.copernicus.org/articles/10/887/2014/cp-10-887-2014.pdf">The full text article is available as a PDF file from https://cp.copernicus.org/articles/10/887/2014/cp-10-887-2014.pdf</self-uri>
<abstract>
<p>In order to reconstruct the temperature of the North Greenland Ice Core
Project (NGRIP) site, new measurements of δ&lt;sup&gt;15&lt;/sup&gt;N have been performed
covering the time period from the beginning of the Holocene to
Dansgaard–Oeschger (DO) event 8. Together with previously measured and
mostly published δ&lt;sup&gt;15&lt;/sup&gt;N data, we present for the first time a NGRIP
temperature reconstruction for the whole last glacial period from 10 to
120 kyr b2k (thousand years before 2000 AD) including every DO event based
on δ&lt;sup&gt;15&lt;/sup&gt;N isotope measurements combined with a firn densification and
heat diffusion model. The detected temperature rises at the onset of DO
events range from 5 °C (DO 25) up to 16.5 °C (DO 11) with an
uncertainty of ±3 °C. To bring measured and modelled data into
agreement, we had to reduce the accumulation rate given by the NGRIP
ss09sea06bm timescale in some periods by 30 to 35%, especially during the
last glacial maximum. A comparison between reconstructed temperature and
δ&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;ice&lt;/sub&gt; data confirms that the isotopic composition of
the stadial was strongly influenced by seasonality. We evidence
an anticorrelation between the variations of the
δ&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;ice&lt;/sub&gt; sensitivity to temperature (referred to as
α) and obliquity in agreement with a simple Rayleigh distillation
model. Finally, we suggest that α might be influenced by the Northern
Hemisphere ice sheet volume.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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