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Glacier acceleration and thinning after ice shelf collapse in the Larsen B embayment, Antarctica

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Scambos, T. A., Bohlander, J. A., Shuman, C. A., Skvarca, P.·2004·Geophysical Research Letters

Abstract

Ice velocities derived from five Landsat 7 images acquired between January 2000 and February 2003 show a two‐ to six‐fold increase in centerline speed of four glaciers flowing into the now‐collapsed section of the Larsen B Ice Shelf. Satellite laser altimetry from ICESat indicates the surface of Hektoria Glacier lowered by up to 38 ± 6 m in a six‐month period beginning one year after the break‐up in March 2002. Smaller elevation losses are observed for Crane and Jorum glaciers over a later 5‐month period. Two glaciers south of the collapse area, Flask and Leppard, show little change in speed or elevation. Seasonal variations in speed preceding the large post‐collapse velocity increases suggest that both summer melt percolation and changes in the stress field due to shelf removal play a major role in glacier dynamics.

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Metadata

Authors
Scambos, T. A., Bohlander, J. A., Shuman, C. A., & Skvarca, P.
Venue
Geophysical Research Letters
Published
2004-09
Volume
31
Issue
18
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2084481702
Cited by
937
References
0
FWCI
15.41
Type
journal article
Language
en
Open access
green

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CoChat. (2026). Citation check: Glacier acceleration and thinning after ice shelf collapse in the Larsen B embayment, Antarctica. https://app.cochat.ai/papers/10.1029/2004gl020670
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Scambos, T. A., Bohlander, J. A., Shuman, C. A., & Skvarca, P. (2004). Glacier acceleration and thinning after ice shelf collapse in the Larsen B embayment, Antarctica. Geophysical Research Letters. https://doi.org/10.1029/2004gl020670

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