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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>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/cpd-6-2055-2010</article-id>
<title-group>
<article-title>Technical Note: Multi-centennial scale analysis and synthesis of an ensemble mean response of ENSO to solar and volcanic forcings</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>SÃ¡nchez-Sesma</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Instituto Mexicano de TecnologÃ­a del Agua, MÃ©xico</addr-line>
</aff>
<pub-date pub-type="epub">
<day>05</day>
<month>10</month>
<year>2010</year>
</pub-date>
<volume>6</volume>
<issue>5</issue>
<fpage>2055</fpage>
<lpage>2069</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>The response of El NiÃ±o Southern Oscillation (ENSO) to solar and
volcanic radiative forcings over the past millennium is reanalyzed and
extrapolated based on historical data and numerical experiments employing
the Zebiakâ€“Cane (ZC) model of the tropical Pacific coupled
oceanâ€“atmosphere system. The results suggest a self-similarity of the
centennial scale component of the reconstructed ENSO record with a shift in
frequencies around 1700 AD when the frequencies almost double. This shift of
regime puts forward the non-linearity of ENSO climate with a possible
centennial scale forecast, suggesting an ENSO trend toward La NiÃ±a
conditions for the next three decades.</p>
</abstract>
<counts><page-count count="15"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
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</article>