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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>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/tcd-3-307-2009</doi>
	<article_url>http://www.the-cryosphere-discuss.net/3/307/2009/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/3/307/2009/tcd-3-307-2009.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/3/307/2009/tcd-3-307-2009.pdf</fulltext_pdf>
	<start_page>307</start_page>
	<end_page>321</end_page>
	<publication_date>2009-04-28</publication_date>
	<article_title content_type="html">Layer disturbances and the radio-echo free zone in ice sheets</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. Drews</name>
			<email>reinhard.drews@awi.de</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>O. Eisen</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>I. Hamann</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>S. Kipfstuhl</name>
		</author>
		<author numeration="5" affiliations="1,3">
			<name>A. Lambrecht</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>D. Steinhage</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>F. Wilhelms</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>H. Miller</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Alfred-Wegener-Institut für Polar- und Meeresforschung, Bremerhaven, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Institut für Umweltphysik, Heidelberg, Germany</affiliation>
		<affiliation numeration="3" content_type="html">now at: Bundesanstalt für Geowissenschaften und Rohstoffe, Hannover, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">Radio-echo sounding of the Antarctic and Greenlandic ice sheets often reveals
a layer in the lowest hundreds of meters above bedrock more or less free of
radio echoes, known as the echo-free zone (EFZ). The cause of this feature is
unclear, so far lacking direct evidence for its origin. We compare echoes
around the EPICA drill site in Dronning Maud Land, Antarctica, with the
microstructural and dielectrical properties of the EPICA-DML ice core. We
find that echoes disappear in the depth range, where the coherency of the
layers is lost due to disturbances caused by the ice flow. At the drill site,
the EFZ onset at ~2100 m marks a boundary, below which the ice core may
have experienced flow induced disturbances on various scales. The dating of
the climate record becomes increasingly difficult below 1900 m, until
correlation with the Dome C record is lost below 2417 m depth. The onset
also indicates changing rheology which needs to be accounted for in the
modeling of ice sheet dynamics.</abstract>
	<references>
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</article>

