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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>3</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/tcd-3-351-2009</doi>
	<article_url>http://www.the-cryosphere-discuss.net/3/351/2009/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/3/351/2009/tcd-3-351-2009.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/3/351/2009/tcd-3-351-2009.pdf</fulltext_pdf>
	<start_page>351</start_page>
	<end_page>381</end_page>
	<publication_date>2009-06-29</publication_date>
	<article_title content_type="html">Mapping and morphometric analysis of 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>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Geography, Physical Geography, University of Wuerzburg, Am Hubland, 97074 Wuerzburg, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">This study provides mapping and analysis of the maximum glacier extent
during the &quot;Little Ice Age&quot; in Jotunheimen, Southern Norway, on a regional scale.
Remote sensing techniques were used to map the glacier area at the maximum of the
&quot;Little Ice Age&quot; (mid 18th century AD). For validation of the mapping,
interpretation of existing glaciochronological studies, analysis of geomorphological maps and
our own field measurements using GPS have been applied. The flow length of the
glaciers and other inventory data were determined by using a Geographical Information
System and a digital elevation model. A total of 233 glaciers existed during
the &quot;Little Ice Age&quot; maximum in Jotunheimen, comprising an overall glacier area of about
290 km&lt;sup&gt;2&lt;/sup&gt;. Mean glacier flow length was calculated as about 1.6 km. Until AD 2003,
the area shrank by about 35% and the mean flow length decreased by about
34%, compared with the maximum &quot;Little Ice Age&quot; extent.</abstract>
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</article>

