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<!DOCTYPE article SYSTEM "http://www.clim-past-discuss.net/inc/cpd/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>2</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/cpd-2-1001-2006</doi>
	<article_url>http://www.clim-past-discuss.net/2/1001/2006/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/2/1001/2006/cpd-2-1001-2006.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/2/1001/2006/cpd-2-1001-2006.pdf</fulltext_pdf>
	<start_page>1001</start_page>
	<end_page>1049</end_page>
	<publication_date>2006-10-26</publication_date>
	<article_title content_type="html">Millennial temperature reconstruction intercomparison and evaluation</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. N. Juckes</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>M. R. Allen</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>K. R. Briffa</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>J. Esper</name>
		</author>
		<author numeration="5" affiliations="5">
			<name>G. C. Hegerl</name>
		</author>
		<author numeration="6" affiliations="6">
			<name>A. Moberg</name>
		</author>
		<author numeration="7" affiliations="3">
			<name>T. J. Osborn</name>
		</author>
		<author numeration="8" affiliations="7">
			<name>S. L. Weber</name>
		</author>
		<author numeration="9" affiliations="8">
			<name>E. Zorita</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">British Atmospheric Data Centre, Rutherford Appleton Laboratory, UK</affiliation>
		<affiliation numeration="2" content_type="html">Atmospheric, Oceanic and Planetary Physics, University of Oxford, UK</affiliation>
		<affiliation numeration="3" content_type="html">Climatic Research Unit, University of East Anglia, UK</affiliation>
		<affiliation numeration="4" content_type="html">Swiss Federal Research Institute for Forest, Snow and Landscape, Bern University, Switzerland</affiliation>
		<affiliation numeration="5" content_type="html">Dept. Earth and Ocean Sciences, Duke University, NC, USA</affiliation>
		<affiliation numeration="6" content_type="html">Department of Meteorology, Stockholm University, Sweden</affiliation>
		<affiliation numeration="7" content_type="html">Royal Netherlands Meteorological Institute (KNMI), De Bilt, The Netherlands</affiliation>
		<affiliation numeration="8" content_type="html">GKSS Research Centre, Geesthacht, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">There has been considerable recent interest in paleoclimate reconstructions of the temperature history of
the last millennium. A wide variety of techniques have been used.
The interrelation between the techniques is sometimes unclear, as different studies often
use distinct data sources as well as distinct methodologies.
Recent work is reviewed with an aim to clarifying the import of
the different approaches.
A range of proxy data collections used by different authors are passed
through two reconstruction algorithms: firstly, inverse regression and,
secondly, compositing followed by variance matching.
It is found that the first method tends to give large weighting to
a small number of proxies and that the second approach is more robust
to varying proxy input.
A reconstruction using 18 proxy records extending back to AD&amp;nbsp;1000 shows a
maximum pre-industrial temperature of 0.25 K (relative to the 1866 to 1970 mean).
The standard error on this estimate, based on the residual in the calibration
period is 0.149 K. Two recent years (1998 and 2005) have exceeded the estimated pre-industrial
maximum by more than 4 standard errors.</abstract>
	<references>
	</references>
</article>

