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<front>
<journal-meta>
<journal-id journal-id-type="publisher">TC</journal-id>
<journal-title-group>
<journal-title>The Cryosphere</journal-title>
<abbrev-journal-title abbrev-type="publisher">TC</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">The Cryosphere</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1994-0424</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/tc-7-1333-2013</article-id>
<title-group>
<article-title>&lt;i&gt;Brief Communication&lt;/i&gt; &quot;The 2013 Erebus Glacier Tongue calving event&quot;</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Stevens</surname>
<given-names>C. L.</given-names>
<ext-link>https://orcid.org/0000-0002-4730-6985</ext-link>
</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>Sirguey</surname>
<given-names>P.</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>Leonard</surname>
<given-names>G. H.</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>Haskell</surname>
<given-names>T. G.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>National Institute for Water and Atmospheric Research (NIWA), Greta Point Wellington, New Zealand</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>University of Auckland, Dept. Physics, New Zealand</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>National School of Surveying, University of Otago, Dunedin, New Zealand</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Callaghan Innovation, Gracefield Lower Hutt, New Zealand</addr-line>
</aff>
<pub-date pub-type="epub">
<day>02</day>
<month>09</month>
<year>2013</year>
</pub-date>
<volume>7</volume>
<issue>5</issue>
<fpage>1333</fpage>
<lpage>1337</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 C. L. Stevens 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://tc.copernicus.org/articles/7/1333/2013/tc-7-1333-2013.html">This article is available from https://tc.copernicus.org/articles/7/1333/2013/tc-7-1333-2013.html</self-uri>
<self-uri xlink:href="https://tc.copernicus.org/articles/7/1333/2013/tc-7-1333-2013.pdf">The full text article is available as a PDF file from https://tc.copernicus.org/articles/7/1333/2013/tc-7-1333-2013.pdf</self-uri>
<abstract>
<p>The Erebus Glacier Tongue, a small floating glacier in southern McMurdo
Sound, is one of the best-studied ice tongues in Antarctica. Despite this,
its calving on the 27 February 2013 (UTC) was around 10 yr earlier than
previously predicted. The calving was likely a result of ocean currents and
the absence of fast ice. The subsequent trajectory of the newly created
iceberg supports previous descriptions of the surface ocean circulation in
southern McMurdo Sound.</p>
</abstract>
<counts><page-count count="5"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
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</back>
</article>