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<article language="en">
	<journal>
		<journal_title>The Cryosphere</journal_title>
		<journal_url>www.the-cryosphere.net</journal_url>
		<issn>1994-0416</issn>
		<eissn>1994-0424</eissn>
		<volume_number>3</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/tc-3-231-2009</doi>
	<article_url>http://www.the-cryosphere.net/3/231/2009/</article_url>
	<abstract_html>http://www.the-cryosphere.net/3/231/2009/tc-3-231-2009.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere.net/3/231/2009/tc-3-231-2009.pdf</fulltext_pdf>
	<start_page>231</start_page>
	<end_page>243</end_page>
	<publication_date>2009-12-01</publication_date>
	<article_title content_type="html">Mapping glaciers in Jotunheimen, South-Norway, during the &quot;Little Ice Age&quot; maximum</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. Baumann</name>
			<email>sabine.baumann@uni-wuerzburg.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>S. Winkler</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>L. M. Andreassen</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Geography, Physical Geography, University of Wuerzburg, Wuerzburg, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Norwegian Water Resources and Energy Directorate (NVE), Oslo, Norway</affiliation>
	</affiliations>
	<abstract content_type="html">The maximum glacier extent during the &quot;Little Ice Age&quot; (mid 18th century AD)
in Jotunheimen, southern Norway, was mapped using remote sensing techniques.
Interpretation of existing glaciochronological studies, analysis of
geomorphological maps, and own GPS-field measurements were applied for
validation of the mapping. The length of glacier centrelines and other
inventory data were determined using a Geographical Information System (GIS)
and a Digital Elevation Model. &quot;Little Ice Age&quot; maximum extent for a total of
233 glaciers comprising an overall glacier area of about 290 km&lt;sup&gt;2&lt;/sup&gt; was mapped.
Mean length of the centreline was calculated to 1.6 km. Until AD 2003, the
area and length shrank by 35% and 34%, respectively, compared with the
maximum &quot;Little Ice Age&quot; extent.</abstract>
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