West Antarctic sites for subglacial drilling to test for past ice-sheet collapse

<p>Mass loss from the West Antarctic Ice Sheet (WAIS) is increasing, and there is concern that an incipient large-scale deglaciation of the marine basins may already be underway. Measurements of cosmogenic nuclides in subglacial bedrock surfaces have the potential to establish whether and...

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Main Authors: P. Spector, J. Stone, D. Pollard, T. Hillebrand, C. Lewis, J. Gombiner
Format: Article
Language:English
Published: Copernicus Publications 2018-08-01
Series:The Cryosphere
Online Access:https://www.the-cryosphere.net/12/2741/2018/tc-12-2741-2018.pdf
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spelling doaj-b7f8c335ca0748febc3975421883a3d72020-11-24T23:53:29ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242018-08-01122741275710.5194/tc-12-2741-2018West Antarctic sites for subglacial drilling to test for past ice-sheet collapseP. Spector0P. Spector1J. Stone2D. Pollard3T. Hillebrand4C. Lewis5J. Gombiner6Department of Earth and Space Sciences, University of Washington, Seattle, WA, USABerkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA, USADepartment of Earth and Space Sciences, University of Washington, Seattle, WA, USAEarth and Environmental Systems Institute, Pennsylvania State University, University Park, PA, USADepartment of Earth and Space Sciences, University of Washington, Seattle, WA, USACenter for Remote Sensing of Ice Sheets (CReSIS), University of Kansas, Lawrence, KS, USADepartment of Earth and Space Sciences, University of Washington, Seattle, WA, USA<p>Mass loss from the West Antarctic Ice Sheet (WAIS) is increasing, and there is concern that an incipient large-scale deglaciation of the marine basins may already be underway. Measurements of cosmogenic nuclides in subglacial bedrock surfaces have the potential to establish whether and when the marine-based portions of the WAIS deglaciated in the past. However, because most of the bedrock revealed by ice-sheet collapse would remain below sea level, shielded from the cosmic-ray flux, drill sites for subglacial sampling must be located in areas where thinning of the residual ice sheet would expose presently subglacial bedrock surfaces. In this paper we discuss the criteria and considerations for choosing drill sites where subglacial samples will provide maximum information about WAIS extent during past interglacial periods. We evaluate candidate sites in West Antarctica and find that sites located adjacent to the large marine basins of West Antarctica will be most diagnostic of past ice-sheet collapse. There are important considerations for drill site selection on the kilometer scale that can only be assessed by field reconnaissance. As a case study of these considerations, we describe reconnaissance at sites in West Antarctica, focusing on the Pirrit Hills, where in the summer of 2016–2017 an 8&thinsp;m bedrock core was retrieved from below 150&thinsp;m of ice.</p>https://www.the-cryosphere.net/12/2741/2018/tc-12-2741-2018.pdf
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language English
format Article
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author P. Spector
P. Spector
J. Stone
D. Pollard
T. Hillebrand
C. Lewis
J. Gombiner
spellingShingle P. Spector
P. Spector
J. Stone
D. Pollard
T. Hillebrand
C. Lewis
J. Gombiner
West Antarctic sites for subglacial drilling to test for past ice-sheet collapse
The Cryosphere
author_facet P. Spector
P. Spector
J. Stone
D. Pollard
T. Hillebrand
C. Lewis
J. Gombiner
author_sort P. Spector
title West Antarctic sites for subglacial drilling to test for past ice-sheet collapse
title_short West Antarctic sites for subglacial drilling to test for past ice-sheet collapse
title_full West Antarctic sites for subglacial drilling to test for past ice-sheet collapse
title_fullStr West Antarctic sites for subglacial drilling to test for past ice-sheet collapse
title_full_unstemmed West Antarctic sites for subglacial drilling to test for past ice-sheet collapse
title_sort west antarctic sites for subglacial drilling to test for past ice-sheet collapse
publisher Copernicus Publications
series The Cryosphere
issn 1994-0416
1994-0424
publishDate 2018-08-01
description <p>Mass loss from the West Antarctic Ice Sheet (WAIS) is increasing, and there is concern that an incipient large-scale deglaciation of the marine basins may already be underway. Measurements of cosmogenic nuclides in subglacial bedrock surfaces have the potential to establish whether and when the marine-based portions of the WAIS deglaciated in the past. However, because most of the bedrock revealed by ice-sheet collapse would remain below sea level, shielded from the cosmic-ray flux, drill sites for subglacial sampling must be located in areas where thinning of the residual ice sheet would expose presently subglacial bedrock surfaces. In this paper we discuss the criteria and considerations for choosing drill sites where subglacial samples will provide maximum information about WAIS extent during past interglacial periods. We evaluate candidate sites in West Antarctica and find that sites located adjacent to the large marine basins of West Antarctica will be most diagnostic of past ice-sheet collapse. There are important considerations for drill site selection on the kilometer scale that can only be assessed by field reconnaissance. As a case study of these considerations, we describe reconnaissance at sites in West Antarctica, focusing on the Pirrit Hills, where in the summer of 2016–2017 an 8&thinsp;m bedrock core was retrieved from below 150&thinsp;m of ice.</p>
url https://www.the-cryosphere.net/12/2741/2018/tc-12-2741-2018.pdf
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