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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ESDD</journal-id>
<journal-title-group>
<journal-title>Earth System Dynamics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ESDD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Earth Syst. Dynam. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">2190-4995</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/esdd-3-979-2012</article-id>
<title-group>
<article-title>Toward a classification of the Central Pacific El Niño</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pascolini-Campbell</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>Zanchettin</surname>
<given-names>D.</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>Bothe</surname>
<given-names>O.</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>Timmreck</surname>
<given-names>C.</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>Matei</surname>
<given-names>D.</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>Jungclaus</surname>
<given-names>J. H.</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>Graf</surname>
<given-names>H.-F.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Max Planck Institute for Meteorology, Hamburg, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>University of Hamburg, KlimaCampus, Hamburg, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>University of Cambridge, Cambridge, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>03</day>
<month>09</month>
<year>2012</year>
</pub-date>
<volume>3</volume>
<issue>2</issue>
<fpage>979</fpage>
<lpage>998</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2012 M. Pascolini-Campbell et al.</copyright-statement>
<copyright-year>2012</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://esd.copernicus.org/preprints/3/979/2012/esdd-3-979-2012.html">This article is available from https://esd.copernicus.org/preprints/3/979/2012/esdd-3-979-2012.html</self-uri>
<self-uri xlink:href="https://esd.copernicus.org/preprints/3/979/2012/esdd-3-979-2012.pdf">The full text article is available as a PDF file from https://esd.copernicus.org/preprints/3/979/2012/esdd-3-979-2012.pdf</self-uri>
<abstract>
<p>We investigate the various methods currently available for distinguishing
between the Central Pacific (CP) El Niño (or &quot;El Niño Modoki&quot;) and
the canonical El Niño by considering 10 different methods and 5 sea
surface temperature (SST) datasets from 1880 to 2010. Years which are
classified as CP El Niños with the greatest convergence between method
and SST dataset are considered to provide a more robust identification of
these events. The results identify 13 yr which are classified the most
consistently as CP events: 1885/1886, 1914/1915, 1940/1941, 1958/1959, 1963/1964,
1968/1969, 1977/1978, 1986/1987, 1991/1992, 2002/2003, 2003/2004, 2004/2005 and 2009/2010.
Our findings also indicate the persistence of CP events throughout the time
period investigated, inciting the role of multidecadal natural climate
variability in generating CP El Niños.</p>
</abstract>
<counts><page-count count="20"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
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