Three-dimensional visualisation of internal layering in Antarctic ice

Over the past 30 years radio-echo sounding (RES) techniques have been used extensively in Antarctica to identify the ice thickness, subglacial conditions and internal layers, which commonly act as stratigraphic markers, or isochrons, within ice sheets. Internal layering thus has significant potentia...

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Main Authors: Bingham, RG, Siegert, MJ
Format: Other Non-Article Part of Journal/Newspaper
Language:English
Published: 2005
Subjects:
Online Access:http://hdl.handle.net/1983/f7bb49d6-5cf8-45ed-878a-c587724c9f93
https://research-information.bris.ac.uk/en/publications/f7bb49d6-5cf8-45ed-878a-c587724c9f93
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spelling ftubristolcris:oai:research-information.bris.ac.uk:publications/f7bb49d6-5cf8-45ed-878a-c587724c9f93 2023-05-15T13:57:49+02:00 Three-dimensional visualisation of internal layering in Antarctic ice Bingham, RG Siegert, MJ 2005 http://hdl.handle.net/1983/f7bb49d6-5cf8-45ed-878a-c587724c9f93 https://research-information.bris.ac.uk/en/publications/f7bb49d6-5cf8-45ed-878a-c587724c9f93 eng eng info:eu-repo/semantics/restrictedAccess Bingham , RG & Siegert , MJ 2005 , Three-dimensional visualisation of internal layering in Antarctic ice . in Polar Regions and Quaternary Climate, European Science Foundation Research Conference, Acqufredda di Maratea, Naples, Italy . contributionToPeriodical 2005 ftubristolcris 2021-08-02T09:53:14Z Over the past 30 years radio-echo sounding (RES) techniques have been used extensively in Antarctica to identify the ice thickness, subglacial conditions and internal layers, which commonly act as stratigraphic markers, or isochrons, within ice sheets. Internal layering thus has significant potential to impart crucial information on the spatial and temporal response of the both the East and West Antarctic ice sheets to climate change. However, to date the analysis and representation of RES data has largely been restricted to two-dimensional applications, such as correlating between two ice-coring sites, and the full potential of RES data for exploring the three-dimensional response of the ice sheet to climate change has yet to be realised. As a first step in addressing this issue, we are developing a fully three-dimensional visualisation of the architecture of the Antarctic Ice Sheet, to provide a powerful new base against which to test numerical reconstructions and predictions. We report here on the three-dimensional structure of Antarctica as reconstructed from RES data collected by SPRI between 1974 and 1978. Over the past 30 years radio-echo sounding (RES) techniques have been used extensively in Antarctica to identify the ice thickness, subglacial conditions and internal layers, which commonly act as stratigraphic markers, or isochrons, within ice sheets. Internal layering thus has significant potential to impart crucial information on the spatial and temporal response of the both the East and West Antarctic ice sheets to climate change. However, to date the analysis and representation of RES data has largely been restricted to two-dimensional applications, such as correlating between two ice-coring sites, and the full potential of RES data for exploring the three-dimensional response of the ice sheet to climate change has yet to be realised. As a first step in addressing this issue, we are developing a fully three-dimensional visualisation of the architecture of the Antarctic Ice Sheet, to provide a powerful new base against which to test numerical reconstructions and predictions. We report here on the three-dimensional structure of Antarctica as reconstructed from RES data collected by SPRI between 1974 and 1978. Other Non-Article Part of Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet University of Bristol: Bristol Research Antarctic The Antarctic
institution Open Polar
collection University of Bristol: Bristol Research
op_collection_id ftubristolcris
language English
description Over the past 30 years radio-echo sounding (RES) techniques have been used extensively in Antarctica to identify the ice thickness, subglacial conditions and internal layers, which commonly act as stratigraphic markers, or isochrons, within ice sheets. Internal layering thus has significant potential to impart crucial information on the spatial and temporal response of the both the East and West Antarctic ice sheets to climate change. However, to date the analysis and representation of RES data has largely been restricted to two-dimensional applications, such as correlating between two ice-coring sites, and the full potential of RES data for exploring the three-dimensional response of the ice sheet to climate change has yet to be realised. As a first step in addressing this issue, we are developing a fully three-dimensional visualisation of the architecture of the Antarctic Ice Sheet, to provide a powerful new base against which to test numerical reconstructions and predictions. We report here on the three-dimensional structure of Antarctica as reconstructed from RES data collected by SPRI between 1974 and 1978. Over the past 30 years radio-echo sounding (RES) techniques have been used extensively in Antarctica to identify the ice thickness, subglacial conditions and internal layers, which commonly act as stratigraphic markers, or isochrons, within ice sheets. Internal layering thus has significant potential to impart crucial information on the spatial and temporal response of the both the East and West Antarctic ice sheets to climate change. However, to date the analysis and representation of RES data has largely been restricted to two-dimensional applications, such as correlating between two ice-coring sites, and the full potential of RES data for exploring the three-dimensional response of the ice sheet to climate change has yet to be realised. As a first step in addressing this issue, we are developing a fully three-dimensional visualisation of the architecture of the Antarctic Ice Sheet, to provide a powerful new base against which to test numerical reconstructions and predictions. We report here on the three-dimensional structure of Antarctica as reconstructed from RES data collected by SPRI between 1974 and 1978.
format Other Non-Article Part of Journal/Newspaper
author Bingham, RG
Siegert, MJ
spellingShingle Bingham, RG
Siegert, MJ
Three-dimensional visualisation of internal layering in Antarctic ice
author_facet Bingham, RG
Siegert, MJ
author_sort Bingham, RG
title Three-dimensional visualisation of internal layering in Antarctic ice
title_short Three-dimensional visualisation of internal layering in Antarctic ice
title_full Three-dimensional visualisation of internal layering in Antarctic ice
title_fullStr Three-dimensional visualisation of internal layering in Antarctic ice
title_full_unstemmed Three-dimensional visualisation of internal layering in Antarctic ice
title_sort three-dimensional visualisation of internal layering in antarctic ice
publishDate 2005
url http://hdl.handle.net/1983/f7bb49d6-5cf8-45ed-878a-c587724c9f93
https://research-information.bris.ac.uk/en/publications/f7bb49d6-5cf8-45ed-878a-c587724c9f93
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
op_source Bingham , RG & Siegert , MJ 2005 , Three-dimensional visualisation of internal layering in Antarctic ice . in Polar Regions and Quaternary Climate, European Science Foundation Research Conference, Acqufredda di Maratea, Naples, Italy .
op_rights info:eu-repo/semantics/restrictedAccess
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