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<article language="en">
	<journal>
		<journal_title>The Cryosphere Discussions</journal_title>
		<journal_url>www.the-cryosphere-discuss.net</journal_url>
		<issn>1994-0432</issn>
		<eissn>1994-0440</eissn>
		<volume_number>1</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/tcd-1-77-2007</doi>
	<article_url>http://www.the-cryosphere-discuss.net/1/77/2007/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/1/77/2007/tcd-1-77-2007.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/1/77/2007/tcd-1-77-2007.pdf</fulltext_pdf>
	<start_page>77</start_page>
	<end_page>97</end_page>
	<publication_date>2007-06-27</publication_date>
	<article_title content_type="html">Reconstructing the glacier contribution to sea-level rise back to 1850</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. Oerlemans</name>
			<email>j.oerlemans@phys.uu.nl</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>M. Dyurgerov</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>R. S. W. van de Wal</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute for Marine and Atmospheric Research, Utrecht University, Princetonplein 5, Utrecht 3584CC, The Netherlands</affiliation>
		<affiliation numeration="2" content_type="html">Department of Physical Geography and Quaternary Geology, Stockholm University, 10654 Stockholm, Sweden</affiliation>
	</affiliations>
	<abstract content_type="html">We present a method to estimate the glacier contribution to sea-level rise
from glacier length records. These records form the only direct evidence of
glacier changes prior to 1946, when the first systematic mass-balance
observations began. A globally representative length signal is calculated
from 197 length records from all continents by normalisation and averaging
of 14 different regions. Next, the resulting signal is calibrated with
mass-balance observations for the period 1961&amp;ndash;2000. We find that the glacier
contribution to sea level rise was 5.5&amp;plusmn;1.0 cm during the period 1850&amp;ndash;2000 and 4.5&amp;plusmn;0.7 cm 
during the period 1900&amp;ndash;2000.</abstract>
	<references>
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</article>

