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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>6</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2012</publication_year>
	</journal>
	<doi>10.5194/tcd-6-159-2012</doi>
	<article_url>http://www.the-cryosphere-discuss.net/6/159/2012/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/6/159/2012/tcd-6-159-2012.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/6/159/2012/tcd-6-159-2012.pdf</fulltext_pdf>
	<start_page>159</start_page>
	<end_page>170</end_page>
	<publication_date>2012-01-17</publication_date>
	<article_title content_type="html">Brief Communication &quot;Importance of slope-induced error correction in elevation change estimates from radar altimetry&quot;</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. T. W. L. Hurkmans</name>
			<email>ruud.hurkmans@bristol.ac.uk</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. L. Bamber</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>J. A. Griggs</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Bristol Glaciology Centre, School of Geographical Sciences, University of Bristol, Bristol, UK</affiliation>
	</affiliations>
	<abstract content_type="html">In deriving elevation change rates (&lt;i&gt;dH/dt&lt;/i&gt;) from radar altimetry, the
      slope-induced error is usually assumed to cancel out in repeat
      measurements. These measurements, however, represent a location that
      can be significantly further upslope than assumed, causing an
      underestimate of the basin-integrated volume change. In a case-study
      for the fast-flowing part of Jakobshavn Isbræ, we show that
      a relatively straightforward correction for slope-induced error
      increases elevation change rates by several metres and increases the
      volume change by 32% for the region of interest.</abstract>
	<references>
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</article>

