Widespread Persistent Thickening of the East Antarctic Ice Sheet by Freezing from the Base-Reference-Cited by-同舟云学术

Widespread Persistent Thickening of the East Antarctic Ice Sheet by Freezing from the Base

Published:2011-03-25 Issue:6024 Volume:331 Page:1592-1595
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Bell Robin E.¹,Ferraccioli Fausto²,Creyts Timothy T.¹,Braaten David³,Corr Hugh²,Das Indrani¹,Damaske Detlef⁴,Frearson Nicholas¹,Jordan Thomas²,Rose Kathryn²,Studinger Michael⁵,Wolovick Michael¹

Affiliation:

1. Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA.

2. British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK.

3. Center for the Remote Sensing of Ice Sheets, Kansas University, Lawrence, KS, USA.

4. Bundesanstalt für Geowissenschaften und Rohstoffe, Hannover, Germany.

5. Goddard Earth Science and Technology Center, University of Maryland Baltimore County, MD, and NASA Goddard Space Flight Center, MD, USA.

Abstract

A large fraction of the ice at Dome A, Antarctica, did not form by the usual process of snowfall compaction.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference13 articles.

1. G. Q. Robin C. W. M. Swithinbank B. M. E. Smith Radio Echo Exploration of the Antarctic Ice Sheet (International Association of Scientific Hydrology Publication 86 1970) pp. 97–115.

2. International studies of ice sheet and bedrock

3. Layer disturbances and the radio-echo free zone in ice sheets

4. Nature of radio echo layering in the Antarctic Ice Sheet detected by a two-frequency experiment

5. Origin and fate of Lake Vostok water frozen to the base of the East Antarctic ice sheet

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