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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>4</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/tcd-4-1225-2010</doi>
	<article_url>http://www.the-cryosphere-discuss.net/4/1225/2010/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/4/1225/2010/tcd-4-1225-2010.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/4/1225/2010/tcd-4-1225-2010.pdf</fulltext_pdf>
	<start_page>1225</start_page>
	<end_page>1241</end_page>
	<publication_date>2010-08-11</publication_date>
	<article_title content_type="html">A comparison of basal reflectivity and ice velocity in East Antarctica</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. W. Jacobel</name>
			<email>jacobel@stolaf.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>K. E. Lapo</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>J. R. Stamp</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>B. W. Youngblood</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>B. C. Welch</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>J. L. Bamber</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Physics, St. Olaf College, Northfield, MN, 55057, USA</affiliation>
		<affiliation numeration="2" content_type="html">School of Geographical Sciences, University of Bristol, Bristol, BS8 1SS, UK</affiliation>
	</affiliations>
	<abstract content_type="html">Ground-based radio echo sounding data acquired along the 1700 km
      US-ITASE traverse have been used to determine ice attenuation and
      relative basal reflectivity across the major catchments funneling ice
      from East Antarctica to the Ross Ice Shelf. We find that basal
      reflectivity varies locally by up to 40 dB which we interpret as due
      to changes in the phase state at the bed. Some, though not all, areas
      of high local reflectivity are observed to have flat-lying bed
      reflections indicative of sub-glacial lakes. We compare basal
      reflectivity to ice balance velocity and find a general association of
      higher flow speeds with high radar reflection strength. This set of
      observations from two independent remotely sensed geophysical data
      sets extends the range of field observations to the interior of East
      Antarctica and confirms the importance of basal lubrication on
      modulating the ice dynamics of the largest ice sheet on the planet.</abstract>
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</article>

