Radio-echo Sounding of Pine Island Glacier, West Antarctica: Understanding the Past from Observations, Analysis and Modelling of Internal Layering

Pine Island Glacier is one of the fastest and most dynamic glaciers in West Antarctica. The stability of the glacier may thus have profound impact on the overall stability of the West Antarctic Ice Sheet and its contribution to global sea-level rise. This thesis addresses questions concerning the pa...

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Main Author: Karlsson, Nanna
Format: Text
Language:English
Published: 2010
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/508259/
https://nora.nerc.ac.uk/id/eprint/508259/1/karlsson_phdthesis2011.pdf
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spelling ftnerc:oai:nora.nerc.ac.uk:508259 2023-05-15T13:48:08+02:00 Radio-echo Sounding of Pine Island Glacier, West Antarctica: Understanding the Past from Observations, Analysis and Modelling of Internal Layering Karlsson, Nanna 2010 text http://nora.nerc.ac.uk/id/eprint/508259/ https://nora.nerc.ac.uk/id/eprint/508259/1/karlsson_phdthesis2011.pdf en eng https://nora.nerc.ac.uk/id/eprint/508259/1/karlsson_phdthesis2011.pdf Karlsson, Nanna. 2010 Radio-echo Sounding of Pine Island Glacier, West Antarctica: Understanding the Past from Observations, Analysis and Modelling of Internal Layering. University of Hull, PhD Thesis. Publication - Thesis NonPeerReviewed 2010 ftnerc 2023-02-04T19:40:11Z Pine Island Glacier is one of the fastest and most dynamic glaciers in West Antarctica. The stability of the glacier may thus have profound impact on the overall stability of the West Antarctic Ice Sheet and its contribution to global sea-level rise. This thesis addresses questions concerning the past dynamics of the glacier using observations of the internal layers in the ice imaged by radio-echo sounding. Results from an extensive internal layer classification showed that no major spatial changes have taken place in the glacier although the analyses did identify signs indicating a past change of flow pattern in several localised areas in the northern part of the catchment basin. Results also indicated that different parts of Pine Island Glacier are likely to respond in different ways to external forcing. The analyses of the radar data were facilitated by the development of new methods for layer classification and tracing. The second part of this thesis focussed on modelling the internal layers using two- and three-dimensional numerical ice flow models. Comparisons between the observed layers and results from the three-dimensional model indicated that a likely change in accumulation rate and pattern had taken place during the past 7 kyr - 17.5 kyr. The model also indicated a time scale for the changes in flow pattern of approximately 6 - 10 kyr. Results from the two-dimensional model further highlighted areas likely to have undergone changes in past ice flow pattern. The results from this study can feed into current efforts to understand the past dynamics of WAIS in order to establish its response to future climate change. Text Antarc* Antarctic Antarctica Ice Sheet Pine Island Pine Island Glacier West Antarctica Natural Environment Research Council: NERC Open Research Archive Antarctic West Antarctica West Antarctic Ice Sheet Pine Island Glacier ENVELOPE(-101.000,-101.000,-75.000,-75.000)
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language English
description Pine Island Glacier is one of the fastest and most dynamic glaciers in West Antarctica. The stability of the glacier may thus have profound impact on the overall stability of the West Antarctic Ice Sheet and its contribution to global sea-level rise. This thesis addresses questions concerning the past dynamics of the glacier using observations of the internal layers in the ice imaged by radio-echo sounding. Results from an extensive internal layer classification showed that no major spatial changes have taken place in the glacier although the analyses did identify signs indicating a past change of flow pattern in several localised areas in the northern part of the catchment basin. Results also indicated that different parts of Pine Island Glacier are likely to respond in different ways to external forcing. The analyses of the radar data were facilitated by the development of new methods for layer classification and tracing. The second part of this thesis focussed on modelling the internal layers using two- and three-dimensional numerical ice flow models. Comparisons between the observed layers and results from the three-dimensional model indicated that a likely change in accumulation rate and pattern had taken place during the past 7 kyr - 17.5 kyr. The model also indicated a time scale for the changes in flow pattern of approximately 6 - 10 kyr. Results from the two-dimensional model further highlighted areas likely to have undergone changes in past ice flow pattern. The results from this study can feed into current efforts to understand the past dynamics of WAIS in order to establish its response to future climate change.
format Text
author Karlsson, Nanna
spellingShingle Karlsson, Nanna
Radio-echo Sounding of Pine Island Glacier, West Antarctica: Understanding the Past from Observations, Analysis and Modelling of Internal Layering
author_facet Karlsson, Nanna
author_sort Karlsson, Nanna
title Radio-echo Sounding of Pine Island Glacier, West Antarctica: Understanding the Past from Observations, Analysis and Modelling of Internal Layering
title_short Radio-echo Sounding of Pine Island Glacier, West Antarctica: Understanding the Past from Observations, Analysis and Modelling of Internal Layering
title_full Radio-echo Sounding of Pine Island Glacier, West Antarctica: Understanding the Past from Observations, Analysis and Modelling of Internal Layering
title_fullStr Radio-echo Sounding of Pine Island Glacier, West Antarctica: Understanding the Past from Observations, Analysis and Modelling of Internal Layering
title_full_unstemmed Radio-echo Sounding of Pine Island Glacier, West Antarctica: Understanding the Past from Observations, Analysis and Modelling of Internal Layering
title_sort radio-echo sounding of pine island glacier, west antarctica: understanding the past from observations, analysis and modelling of internal layering
publishDate 2010
url http://nora.nerc.ac.uk/id/eprint/508259/
https://nora.nerc.ac.uk/id/eprint/508259/1/karlsson_phdthesis2011.pdf
long_lat ENVELOPE(-101.000,-101.000,-75.000,-75.000)
geographic Antarctic
West Antarctica
West Antarctic Ice Sheet
Pine Island Glacier
geographic_facet Antarctic
West Antarctica
West Antarctic Ice Sheet
Pine Island Glacier
genre Antarc*
Antarctic
Antarctica
Ice Sheet
Pine Island
Pine Island Glacier
West Antarctica
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
Pine Island
Pine Island Glacier
West Antarctica
op_relation https://nora.nerc.ac.uk/id/eprint/508259/1/karlsson_phdthesis2011.pdf
Karlsson, Nanna. 2010 Radio-echo Sounding of Pine Island Glacier, West Antarctica: Understanding the Past from Observations, Analysis and Modelling of Internal Layering. University of Hull, PhD Thesis.
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