Progressive unpinning of Thwaites Glacier from newly identified offshore ridge: Constraints from aerogravity-Reference-Cited by-同舟云学术

Progressive unpinning of Thwaites Glacier from newly identified offshore ridge: Constraints from aerogravity

Published:2011-10 Issue:20 Volume:38 Page:n/a-n/a
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Tinto K. J.¹,Bell R. E.¹

Affiliation:

1. Lamont-Doherty Earth Observatory; Earth Institute at Columbia University; Palisades; New York; USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://www.agu.org/journals/gl/gl1120/2011GL049026/2011GL049026.pdf

Reference28 articles.

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4. Velocity measurements and changes in position of Thwaites Glacier/iceberg tongue from aerial photography, Landsat images and NOAA AVHRR data;Ferrigno;Ann. Glaciol.,1993

5. Basement control on past ice sheet dynamics in the Amundsen Sea Embayment, West Antarctica;Gohl;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2011

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