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<article language="en">
	<journal>
		<journal_title>Advances in Geosciences</journal_title>
		<journal_url>www.adv-geosci.net</journal_url>
		<issn>1680-7340</issn>
		<eissn>1680-7359</eissn>
		<volume_number>6</volume_number>
		<volume_title>1st Alexander von Humboldt International Conference</volume_title>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/adgeo-6-173-2006</doi>
	<article_url>http://www.adv-geosci.net/6/173/2006/</article_url>
	<abstract_html>http://www.adv-geosci.net/6/173/2006/adgeo-6-173-2006.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/6/173/2006/adgeo-6-173-2006.pdf</fulltext_pdf>
	<start_page>173</start_page>
	<end_page>179</end_page>
	<publication_date>2006-02-01</publication_date>
	<article_title content_type="html">How unusual was late 20th century El Niño-Southern Oscillation (ENSO)? Assessing evidence from tree-ring, coral, ice-core and documentary palaeoarchives, A.D. 1525-2002</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. L. Gergis</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>A. M. Fowler</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Biological, Earth and Environmental Sci., Univ. of New South Wales, Kensington, NSW 2052, Sydney, Australia</affiliation>
		<affiliation numeration="2" content_type="html">School of Geography and Environmental Science, University of Auckland, Private Bag 92019 Auckland, New Zealand</affiliation>
	</affiliations>
	<abstract content_type="html">Multiple proxy records (tree-ring, coral, ice and documentary) were examined
to isolate ENSO signals associated with both phases of the phenomenon for
the period A.D.&amp;nbsp;1525-2002. To avoid making large-scale inferences from
single proxy analysis, regional signals were aggregated into a network of
high-resolution records, revealing large-scale trends in the frequency,
magnitude and duration of pre-instrumental ENSO using novel applications of
percentile analysis. Here we use the newly introduced coupled
ocean-atmosphere ENSO index (CEI) as a baseline for the calibration of proxy
records. The reconstruction revealed 83 extreme or very strong ENSO episodes
since A.D.&amp;nbsp;1525, expanding considerably on existing ENSO event chronologies.
Significantly, excerpts of the most comprehensive list of La Ni&amp;#241;a events
complied to date are presented, indicating peak activity during the
16th to mid 17th and 20th centuries. Although extreme events
are seen throughout the 478-year reconstruction, 43% of the extreme ENSO
events noted since A.D.&amp;nbsp;1525 occur during the 20th century, with an
obvious bias towards enhanced El Ni&amp;#241;o conditions in recent decades. Of
the total number of extreme event years reconstructed, 30% of all
reconstructed ENSO event years occur post-1940 alone suggesting that recent
ENSO variability appears anomalous in the context of the past five
centuries.</abstract>
	<references>
	</references>
</article>

