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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>1</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/cpd-1-17-2005</doi>
	<article_url>http://www.clim-past-discuss.net/1/17/2005/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/1/17/2005/cpd-1-17-2005.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/1/17/2005/cpd-1-17-2005.pdf</fulltext_pdf>
	<start_page>17</start_page>
	<end_page>56</end_page>
	<publication_date>2005-07-25</publication_date>
	<article_title content_type="html">Where can the Arctic oscillation be reconstructed? Towards a reconstruction of climate modes based on stable teleconnections</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G. Lohmann</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>N. Rimbu</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. Dima</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">Proxy data can bring observed climate variability of the last 100 years
 into a long-term context. We identify regions of the Northern Hemisphere
where the teleconnection patterns of the Arctic Oscillation are stationary.
Our method provides a systematic way to examine optimal sites for the reconstruction of climate modes based on
paleoclimatic archives that sensitively record temperature and precipitation variations.
We identify the regions for boreal winter and spring that
can be used to reconstruct the Arctic Oscillation index in the pre-instrumental period.
Finally, this technique is applied to high resolution
coral, tree ring, ice core and mollusk shell data to understand proxy-climate teleconnections and their use for climate reconstructions.</abstract>
	<references>
	</references>
</article>

