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<front>
<journal-meta>
<journal-id journal-id-type="publisher">CPD</journal-id>
<journal-title-group>
<journal-title>Climate of the Past Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">CPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1814-9359</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/cpd-8-1089-2012</article-id>
<title-group>
<article-title>On the gas-ice depth difference (&amp;Delta;depth) along the EPICA Dome C ice core</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Parrenin</surname>
<given-names>F.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Barker</surname>
<given-names>S.</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>Blunier</surname>
<given-names>T.</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>Chappellaz</surname>
<given-names>J.</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>Jouzel</surname>
<given-names>J.</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>Landais</surname>
<given-names>A.</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>Masson-Delmotte</surname>
<given-names>V.</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>Schwander</surname>
<given-names>J.</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>Veres</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Laboratoire Chrono-Environnement, Besançon, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>UJF Grenoble 1,  UMR5183, CNRS &amp;ndash; Laboratoire de Glaciologie et Géophysique de l&apos;Environnement (LGGE), Grenoble F38041, France</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>School of Earth and Ocean Sciences, Cardiff University, UK</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Laboratoire des Sciences du Climat et de l&apos;Environnement, Gif-sur-Yvette, France</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Physics Institute, University of Bern, Bern, Switzerland</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Institute of Speleology, Romanian Academy, Cluj-Napoca, Romania</addr-line>
</aff>
<pub-date pub-type="epub">
<day>03</day>
<month>04</month>
<year>2012</year>
</pub-date>
<volume>8</volume>
<issue>2</issue>
<fpage>1089</fpage>
<lpage>1131</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>
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<self-uri xlink:href="http://www.clim-past-discuss.net/8/1089/2012/cpd-8-1089-2012.pdf">The full text article is available as a PDF file from http://www.clim-past-discuss.net/8/1089/2012/cpd-8-1089-2012.pdf</self-uri>
<abstract>
<p>We compare a variety of methods for estimating the gas/ice depth offset
(&amp;Delta;depth) at EPICA Dome C (EDC, East Antarctica). (1) Purely based on
modelling efforts, &amp;Delta;depth can be estimated combining a firn
densification with an ice flow model. Observations allow direct and indirect
estimate of &amp;Delta;depth. (2) The diffusive column height can be estimated
from &amp;delta;&lt;sup&gt;15&lt;/sup&gt;N and converted to &amp;Delta;depth using an ice flow
model and assumptions about past average firn density and thickness of the
convective zone. (3) Ice and gas synchronisation of the EDC ice core to the
GRIP, EDML and TALDICE ice cores shifts the ice/gas offset problem into
higher accumulation ice cores where it can be more accurately evaluated. (4) Finally, the bipolar seesaw hypothesis allows us to synchronise the ice
isotopic record with the gas CH&lt;sub&gt;4&lt;/sub&gt; record, the later being taken as a
proxy of Greenland temperature. The bipolar seesaw antiphase relationship is
generally supported by the ice-gas cross synchronisation between EDC and the
GRIP, EDML and TALDICE ice cores, which provide support for method 4.
Applying the bipolar seesaw hypothesis to the deeper section of the EDC core
confirms that the ice flow is complex and can help improving our
reconstruction of the thinning function and thus of the EDC age scale. We
confirm that method 1 overestimates the glacial &amp;Delta;depth at EDC and we
suggested that it is due to an overestimation of the glacial Close Off Depth
by the firn densification model. In contrast we find that the glaciological
models probably underestimate the &amp;Delta;depth during termination II.
Finally, we show that method 2 based on &lt;sup&gt;15&lt;/sup&gt;N data produces for the last
deglaciation a &amp;Delta;depth estimate which is in good agreement with
methods 3 and 4.</p>
</abstract>
<counts><page-count count="43"/></counts>
</article-meta>
</front>
<body/>
<back>
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