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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-8-1319-2012</article-id>
<title-group>
<article-title>Influence of LGM boundary conditions on the global water isotope distribution in an atmospheric  general circulation model</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tharammal</surname>
<given-names>T.</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>Paul</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<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>Merkel</surname>
<given-names>U.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</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>Noone</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Geosciences, University of Bremen, Bremen, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>European Graduate College &quot;Proxies in Earth History&quot; (EUROPROX), University of Bremen, Bremen, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>MARUM &amp;ndash; Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Atmospheric and Oceanic Sciences and Cooperative Institute for Research in  Environmental Sciences, University of Colorado, Boulder, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>18</day>
<month>04</month>
<year>2012</year>
</pub-date>
<volume>8</volume>
<issue>2</issue>
<fpage>1319</fpage>
<lpage>1368</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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<abstract>
<p>A series of experiments was conducted using a water isotope tracers-enabled atmospheric general
  circulation model (Community Atmosphere Model version 3.0, CAM3.0-Iso), by changing the individual
  boundary conditions (greenhouse gases, ice sheet albedo and topography, sea-surface temperature)
  each at a time to Last Glacial Maximum (LGM) values. In addition, a combined simulation with all
  the boundary conditions being set to LGM values was carried out. A pre-industrial (PI) simulation
  with boundary conditions taken according to the PMIP2 (Paleoclimate Modelling Intercomparison
  Project) protocol was performed as the control experiment. The experiments were designed in order
  to analyze the temporal and spatial variations of the oxygen isotopic composition of precipitation
  (&amp;delta;&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;precip&lt;/sub&gt;) in response to individual climate factors. The change in
  topography (due to the change in land-ice cover) played a significant role in reducing the surface
  temperature and &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;precip&lt;/sub&gt; over North America.  Exposed shelf areas
  and the ice sheet albedo reduced the Northern Hemisphere surface temperature and &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;precip&lt;/sub&gt; further. A global mean cooling of 4.1 &amp;deg;C was simulated with combined LGM boundary conditions compared to the control simulation, which was in agreement
  with previous experiments using the fully coupled Community Climate System Model (CCSM3).  Large
  reductions in &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;precip&lt;/sub&gt; over the LGM ice sheets were highly
  correlated with the temperature decrease over them. The SST and ice sheet topography changes were
  found to be responsible for most of the changes in the climate and hence the &amp;delta;&lt;sup&gt;18&lt;/sup&gt;O&lt;sub&gt;precip&lt;/sub&gt; distribution among the simulations.</p>
</abstract>
<counts><page-count count="50"/></counts>
</article-meta>
</front>
<body/>
<back>
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