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Title: Reactivation of Kamb Ice Stream tributaries triggers century-scale reorganization of Siple Coast ice flow in West Antarctica

Abstract

Ongoing, centennial-scale flow variability within the Ross ice streams of West Antarctica suggests that the present-day positive mass balance in this region may reverse in the future. Here we use a three-dimensional ice sheet model to simulate ice flow in this region over 250 years. The flow responds to changing basal properties, as a subglacial till layer interacts with water transported in an active subglacial hydrological system. We show that a persistent weak bed beneath the tributaries of the dormant Kamb Ice Stream is a source of internal ice flow instability, which reorganizes all ice streams in this region, leading to a reduced (positive) mass balance within decades and a net loss of ice within two centuries. This hitherto unaccounted for flow variability could raise sea level by 5 mm this century. Furthermore, better constraints on future sea level change from this region will require improved estimates of geothermal heat flux and subglacial water transport.

Authors:
 [1];  [1];  [2];  [3];  [4];  [3]
  1. Univ. of Cambridge, Cambridge (United Kingdom)
  2. Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
  3. Univ. of California, San Diego, La Jolla, CA (United States)
  4. Univ. of California, Santa Cruz, CA (United States)
Publication Date:
Research Org.:
Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
Sponsoring Org.:
USDOE
OSTI Identifier:
1255085
Report Number(s):
LA-UR-15-27433
Journal ID: ISSN 0094-8276
Grant/Contract Number:  
NE/E005950/1; NE/J005800/1; 0338295; ANT-0838885; AC52-06NA25396
Resource Type:
Accepted Manuscript
Journal Name:
Geophysical Research Letters
Additional Journal Information:
Journal Volume: 42; Journal Issue: 20; Journal ID: ISSN 0094-8276
Publisher:
American Geophysical Union
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES; 97 MATHEMATICS AND COMPUTING

Citation Formats

Bougamont, M., Christoffersen, P., Price, S. F., Fricker, H. A., Tulaczyk, S., and Carter, S. P. Reactivation of Kamb Ice Stream tributaries triggers century-scale reorganization of Siple Coast ice flow in West Antarctica. United States: N. p., 2015. Web. doi:10.1002/2015GL065782.
Bougamont, M., Christoffersen, P., Price, S. F., Fricker, H. A., Tulaczyk, S., & Carter, S. P. Reactivation of Kamb Ice Stream tributaries triggers century-scale reorganization of Siple Coast ice flow in West Antarctica. United States. https://doi.org/10.1002/2015GL065782
Bougamont, M., Christoffersen, P., Price, S. F., Fricker, H. A., Tulaczyk, S., and Carter, S. P. Wed . "Reactivation of Kamb Ice Stream tributaries triggers century-scale reorganization of Siple Coast ice flow in West Antarctica". United States. https://doi.org/10.1002/2015GL065782. https://www.osti.gov/servlets/purl/1255085.
@article{osti_1255085,
title = {Reactivation of Kamb Ice Stream tributaries triggers century-scale reorganization of Siple Coast ice flow in West Antarctica},
author = {Bougamont, M. and Christoffersen, P. and Price, S. F. and Fricker, H. A. and Tulaczyk, S. and Carter, S. P.},
abstractNote = {Ongoing, centennial-scale flow variability within the Ross ice streams of West Antarctica suggests that the present-day positive mass balance in this region may reverse in the future. Here we use a three-dimensional ice sheet model to simulate ice flow in this region over 250 years. The flow responds to changing basal properties, as a subglacial till layer interacts with water transported in an active subglacial hydrological system. We show that a persistent weak bed beneath the tributaries of the dormant Kamb Ice Stream is a source of internal ice flow instability, which reorganizes all ice streams in this region, leading to a reduced (positive) mass balance within decades and a net loss of ice within two centuries. This hitherto unaccounted for flow variability could raise sea level by 5 mm this century. Furthermore, better constraints on future sea level change from this region will require improved estimates of geothermal heat flux and subglacial water transport.},
doi = {10.1002/2015GL065782},
journal = {Geophysical Research Letters},
number = 20,
volume = 42,
place = {United States},
year = {Wed Oct 21 00:00:00 EDT 2015},
month = {Wed Oct 21 00:00:00 EDT 2015}
}

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Works referencing / citing this record:

Contrasting Hydrological Controls on Bed Properties During the Acceleration of Pine Island Glacier, West Antarctica
journal, January 2019

  • Bougamont, M.; Christoffersen, P.; Nias, I.
  • Journal of Geophysical Research: Earth Surface, Vol. 124, Issue 1
  • DOI: 10.1029/2018jf004707

Tremor during ice stream stick-slip
journal, January 2015


Antarctic subglacial lakes drain through sediment-floored canals: theory and model testing on real and idealized domains
journal, January 2017

  • Carter, Sasha P.; Fricker, Helen A.; Siegfried, Matthew R.
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Episodic ice velocity fluctuations triggered by a subglacial flood in West Antarctica
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  • Siegfried, Matthew R.; Fricker, Helen A.; Carter, Sasha P.
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Spatially Variable Geothermal Heat Flux in West Antarctica: Evidence and Implications
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Tremor during ice-stream stick slip
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Contrasting hydrological controls on bed properties during the acceleration of Pine Island Glacier, West Antarctica
text, January 2019

  • Bougamont, Marion; Christoffersen, Poul; Nias, Isabel
  • Apollo - University of Cambridge Repository
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Antarctic subglacial lakes drain through sediment-floored canals: Theory and model testing on real and idealized domains
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  • Carter, Sasha P.; Fricker, Helen A.; Siegfried, Matthew R.
  • The Cryosphere
  • DOI: 10.5194/tc-2016-74