Subglacial bed properties from normal-incidence seismic reflection data

Recent applications of the normal-incidence seismic reflection technique to studying subglacial conditions are summarized. Some of the important aspects of the technique are discussed, including critical acquisition parameters and particular strengths and weaknesses. The main reason for deploying th...

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Published in:Journal of Environmental and Engineering Geophysics
Main Author: Smith, Andrew M.
Format: Article in Journal/Newspaper
Language:unknown
Published: Environmental Engineering Geophysical Society 2007
Subjects:
Ice
Online Access:http://nora.nerc.ac.uk/id/eprint/11962/
http://jeeg.geoscienceworld.org/cgi/content/abstract/12/1/3
id ftnerc:oai:nora.nerc.ac.uk:11962
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spelling ftnerc:oai:nora.nerc.ac.uk:11962 2023-12-24T10:09:09+01:00 Subglacial bed properties from normal-incidence seismic reflection data Smith, Andrew M. 2007 http://nora.nerc.ac.uk/id/eprint/11962/ http://jeeg.geoscienceworld.org/cgi/content/abstract/12/1/3 unknown Environmental Engineering Geophysical Society Smith, Andrew M. orcid:0000-0001-8577-482X . 2007 Subglacial bed properties from normal-incidence seismic reflection data. Journal of Environmental and Engineering Geophysics, 12 (1). 3-13. https://doi.org/10.2113/JEEG12.1.3 <https://doi.org/10.2113/JEEG12.1.3> Glaciology Earth Sciences Publication - Article PeerReviewed 2007 ftnerc https://doi.org/10.2113/JEEG12.1.3 2023-11-24T00:03:08Z Recent applications of the normal-incidence seismic reflection technique to studying subglacial conditions are summarized. Some of the important aspects of the technique are discussed, including critical acquisition parameters and particular strengths and weaknesses. The main reason for deploying this technique, rather than other seismic methods, is that data acquisition is simpler and requires fewer resources. Current limitations of the technique include the inability to determine subglacial seismic velocities, uncertainty in the attenuation coefficient for ice, and assumptions of source repeatability. The reflection coefficient at the ice-bed interface is calculated from the energy reduction between primary and multiple reflections. From this, the acoustic impedance of the bed is derived and used to interpret the bed material. Beneath fast-flowing ice, dilatant, deforming sediment has been distinguished from a lodged sediment bed, using porosity as a proxy for sediment dilation. Subglacial water and permafrost have also been interpreted. Data from a number of locations can be used to develop a model of the basal conditions of a complete glacier. Results from sites on ice streams in West Antarctica show how the ice encounters a greater or lesser restraint to flow, from different basal conditions. Application to a glacier in the Arctic, suggests its most recent surge terminated when water escaped through discontinuous permafrost beneath the ice. Further glaciological questions that could be addressed using the technique are proposed. Article in Journal/Newspaper Antarc* Antarctica Arctic Ice permafrost West Antarctica Natural Environment Research Council: NERC Open Research Archive Arctic West Antarctica Journal of Environmental and Engineering Geophysics 12 1 3 13
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
topic Glaciology
Earth Sciences
spellingShingle Glaciology
Earth Sciences
Smith, Andrew M.
Subglacial bed properties from normal-incidence seismic reflection data
topic_facet Glaciology
Earth Sciences
description Recent applications of the normal-incidence seismic reflection technique to studying subglacial conditions are summarized. Some of the important aspects of the technique are discussed, including critical acquisition parameters and particular strengths and weaknesses. The main reason for deploying this technique, rather than other seismic methods, is that data acquisition is simpler and requires fewer resources. Current limitations of the technique include the inability to determine subglacial seismic velocities, uncertainty in the attenuation coefficient for ice, and assumptions of source repeatability. The reflection coefficient at the ice-bed interface is calculated from the energy reduction between primary and multiple reflections. From this, the acoustic impedance of the bed is derived and used to interpret the bed material. Beneath fast-flowing ice, dilatant, deforming sediment has been distinguished from a lodged sediment bed, using porosity as a proxy for sediment dilation. Subglacial water and permafrost have also been interpreted. Data from a number of locations can be used to develop a model of the basal conditions of a complete glacier. Results from sites on ice streams in West Antarctica show how the ice encounters a greater or lesser restraint to flow, from different basal conditions. Application to a glacier in the Arctic, suggests its most recent surge terminated when water escaped through discontinuous permafrost beneath the ice. Further glaciological questions that could be addressed using the technique are proposed.
format Article in Journal/Newspaper
author Smith, Andrew M.
author_facet Smith, Andrew M.
author_sort Smith, Andrew M.
title Subglacial bed properties from normal-incidence seismic reflection data
title_short Subglacial bed properties from normal-incidence seismic reflection data
title_full Subglacial bed properties from normal-incidence seismic reflection data
title_fullStr Subglacial bed properties from normal-incidence seismic reflection data
title_full_unstemmed Subglacial bed properties from normal-incidence seismic reflection data
title_sort subglacial bed properties from normal-incidence seismic reflection data
publisher Environmental Engineering Geophysical Society
publishDate 2007
url http://nora.nerc.ac.uk/id/eprint/11962/
http://jeeg.geoscienceworld.org/cgi/content/abstract/12/1/3
geographic Arctic
West Antarctica
geographic_facet Arctic
West Antarctica
genre Antarc*
Antarctica
Arctic
Ice
permafrost
West Antarctica
genre_facet Antarc*
Antarctica
Arctic
Ice
permafrost
West Antarctica
op_relation Smith, Andrew M. orcid:0000-0001-8577-482X . 2007 Subglacial bed properties from normal-incidence seismic reflection data. Journal of Environmental and Engineering Geophysics, 12 (1). 3-13. https://doi.org/10.2113/JEEG12.1.3 <https://doi.org/10.2113/JEEG12.1.3>
op_doi https://doi.org/10.2113/JEEG12.1.3
container_title Journal of Environmental and Engineering Geophysics
container_volume 12
container_issue 1
container_start_page 3
op_container_end_page 13
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