Reconstructing the history of the Antarctic ice sheet using internal reflecting horizons from radio-echo sounding
Understanding the contribution of the Antarctic Ice Sheet (AIS) to past and future sea-level rise has emerged as a scientific priority over the last four decades. Whilst our knowledge of ice-dynamical changes occurring as a result of current anthropogenic forcing has improved considerably since the...
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Other Authors: | , , , |
Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
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The University of Edinburgh
2023
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Online Access: | https://hdl.handle.net/1842/40725 https://doi.org/10.7488/era/3485 |
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ftunivedinburgh:oai:era.ed.ac.uk:1842/40725 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Edinburgh Research Archive (ERA - University of Edinburgh) |
op_collection_id |
ftunivedinburgh |
language |
English |
topic |
Antarctica radar Internal Reflecting Horizons Volcano ice-sheet models Holocene ice core Thwaites Glacier Pine Island Glacier ice sheet Stratigraphy West Antarctica |
spellingShingle |
Antarctica radar Internal Reflecting Horizons Volcano ice-sheet models Holocene ice core Thwaites Glacier Pine Island Glacier ice sheet Stratigraphy West Antarctica Bodart, Julien Reconstructing the history of the Antarctic ice sheet using internal reflecting horizons from radio-echo sounding |
topic_facet |
Antarctica radar Internal Reflecting Horizons Volcano ice-sheet models Holocene ice core Thwaites Glacier Pine Island Glacier ice sheet Stratigraphy West Antarctica |
description |
Understanding the contribution of the Antarctic Ice Sheet (AIS) to past and future sea-level rise has emerged as a scientific priority over the last four decades. Whilst our knowledge of ice-dynamical changes occurring as a result of current anthropogenic forcing has improved considerably since the start of the satellite era, significantly less is known about the evolution of the AIS during the pre-industrial Holocene (the last ~11.7 thousand years; ka). Quantifying these changes is crucial, however, as this time period corresponds to a time when the ice sheet was retreating from its maximal extent at the Last Glacial Maximum (LGM; ~20 ka) and environmental conditions were similar to today. Therefore, improving our understanding of this period may provide a long-term context to the decadal changes observed in recent times and how these may evolve in the future. Whilst point-based geochronological measurements of ice and sediment cores, or surface exposure dating, can be used to assess past ice-sheet changes over the AIS, it remains unclear how representative they are of a wider region. A complementary and spatially extensive resource across the ice sheet are Internal Reflecting Horizons (IRHs) as imaged by Radio-Echo Sounding (RES) techniques, which provide a cumulative record of accumulation, basal melt and ice dynamics that, if dated precisely at ice cores, can be used to inform numerical ice-sheet models projecting past and future changes on large spatial scales. The aim of this thesis is therefore to develop and extend age-depth models from IRHs across the AIS to assess the past stability of the ice sheet. In this thesis, an age-depth model of Pine Island Glacier spanning the LGM and Holocene periods is derived from spatially extensive IRHs. The connection between RES profiles and the WAIS Divide ice core enables the direct dating of the IRHs, and reveals that they match large peaks in sulphate concentrations which are unparalleled in the 68,000 year-old record, thus suggesting that the cause of these IRHs ... |
author2 |
Bingham, Robert Hein, Andrew Attal, Mikael Natural Environment Research Council (NERC) |
format |
Doctoral or Postdoctoral Thesis |
author |
Bodart, Julien |
author_facet |
Bodart, Julien |
author_sort |
Bodart, Julien |
title |
Reconstructing the history of the Antarctic ice sheet using internal reflecting horizons from radio-echo sounding |
title_short |
Reconstructing the history of the Antarctic ice sheet using internal reflecting horizons from radio-echo sounding |
title_full |
Reconstructing the history of the Antarctic ice sheet using internal reflecting horizons from radio-echo sounding |
title_fullStr |
Reconstructing the history of the Antarctic ice sheet using internal reflecting horizons from radio-echo sounding |
title_full_unstemmed |
Reconstructing the history of the Antarctic ice sheet using internal reflecting horizons from radio-echo sounding |
title_sort |
reconstructing the history of the antarctic ice sheet using internal reflecting horizons from radio-echo sounding |
publisher |
The University of Edinburgh |
publishDate |
2023 |
url |
https://hdl.handle.net/1842/40725 https://doi.org/10.7488/era/3485 |
long_lat |
ENVELOPE(-101.000,-101.000,-75.000,-75.000) ENVELOPE(-106.750,-106.750,-75.500,-75.500) |
geographic |
Antarctic The Antarctic West Antarctica Pine Island Glacier Thwaites Glacier |
geographic_facet |
Antarctic The Antarctic West Antarctica Pine Island Glacier Thwaites Glacier |
genre |
Antarc* Antarctic Antarctica ice core Ice Sheet Pine Island Pine Island Glacier The Cryosphere Thwaites Glacier West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica ice core Ice Sheet Pine Island Pine Island Glacier The Cryosphere Thwaites Glacier West Antarctica |
op_relation |
British Antarctic Survey's aerogeophysical data: releasing 25 years of airborne gravity, magnetic, and radar datasets over Antarctica Frémand, A. C., Bodart, J. A., Jordan, T. A., Ferraccioli, F., Robinson, C., Corr, H. F. J., Peat, H. J., Bingham, R. G. & Vaughan, D. G., 25 Jul 2022, In: Earth System Science Data. 14, 7, p. 3379-3410 Age-Depth Stratigraphy of Pine Island Glacier Inferred from Airborne Radar and Ice-Core Chronology Bodart, J., Bingham, R. G., Ashmore, D. W., Karlsson, N. B., Hein, A. & Vaughan, D. G., 24 Mar 2021, (E-pub ahead of print) In: Journal of Geophysical Research: Earth Surface. High mid-Holocene accumulation rates over West Antarctica inferred from a pervasive ice-penetrating radar reflector Bodart, J. A., Bingham, R. G., Young, D. A., Macgregor, J. A., Ashmore, D. W., Quartini, E., Hein, A. S., Vaughan, D. G. & Blankenship, D. D., 6 Apr 2023, In: The Cryosphere. 17, 4, p. 1497-1512 https://hdl.handle.net/1842/40725 http://dx.doi.org/10.7488/era/3485 |
op_doi |
https://doi.org/10.7488/era/3485 |
_version_ |
1772809772693716992 |
spelling |
ftunivedinburgh:oai:era.ed.ac.uk:1842/40725 2023-07-30T03:59:04+02:00 Reconstructing the history of the Antarctic ice sheet using internal reflecting horizons from radio-echo sounding Bodart, Julien Bingham, Robert Hein, Andrew Attal, Mikael Natural Environment Research Council (NERC) 2023-06-23 application/pdf https://hdl.handle.net/1842/40725 https://doi.org/10.7488/era/3485 en eng The University of Edinburgh British Antarctic Survey's aerogeophysical data: releasing 25 years of airborne gravity, magnetic, and radar datasets over Antarctica Frémand, A. C., Bodart, J. A., Jordan, T. A., Ferraccioli, F., Robinson, C., Corr, H. F. J., Peat, H. J., Bingham, R. G. & Vaughan, D. G., 25 Jul 2022, In: Earth System Science Data. 14, 7, p. 3379-3410 Age-Depth Stratigraphy of Pine Island Glacier Inferred from Airborne Radar and Ice-Core Chronology Bodart, J., Bingham, R. G., Ashmore, D. W., Karlsson, N. B., Hein, A. & Vaughan, D. G., 24 Mar 2021, (E-pub ahead of print) In: Journal of Geophysical Research: Earth Surface. High mid-Holocene accumulation rates over West Antarctica inferred from a pervasive ice-penetrating radar reflector Bodart, J. A., Bingham, R. G., Young, D. A., Macgregor, J. A., Ashmore, D. W., Quartini, E., Hein, A. S., Vaughan, D. G. & Blankenship, D. D., 6 Apr 2023, In: The Cryosphere. 17, 4, p. 1497-1512 https://hdl.handle.net/1842/40725 http://dx.doi.org/10.7488/era/3485 Antarctica radar Internal Reflecting Horizons Volcano ice-sheet models Holocene ice core Thwaites Glacier Pine Island Glacier ice sheet Stratigraphy West Antarctica Thesis or Dissertation Doctoral PhD Doctor of Philosophy 2023 ftunivedinburgh https://doi.org/10.7488/era/3485 2023-07-09T20:29:41Z Understanding the contribution of the Antarctic Ice Sheet (AIS) to past and future sea-level rise has emerged as a scientific priority over the last four decades. Whilst our knowledge of ice-dynamical changes occurring as a result of current anthropogenic forcing has improved considerably since the start of the satellite era, significantly less is known about the evolution of the AIS during the pre-industrial Holocene (the last ~11.7 thousand years; ka). Quantifying these changes is crucial, however, as this time period corresponds to a time when the ice sheet was retreating from its maximal extent at the Last Glacial Maximum (LGM; ~20 ka) and environmental conditions were similar to today. Therefore, improving our understanding of this period may provide a long-term context to the decadal changes observed in recent times and how these may evolve in the future. Whilst point-based geochronological measurements of ice and sediment cores, or surface exposure dating, can be used to assess past ice-sheet changes over the AIS, it remains unclear how representative they are of a wider region. A complementary and spatially extensive resource across the ice sheet are Internal Reflecting Horizons (IRHs) as imaged by Radio-Echo Sounding (RES) techniques, which provide a cumulative record of accumulation, basal melt and ice dynamics that, if dated precisely at ice cores, can be used to inform numerical ice-sheet models projecting past and future changes on large spatial scales. The aim of this thesis is therefore to develop and extend age-depth models from IRHs across the AIS to assess the past stability of the ice sheet. In this thesis, an age-depth model of Pine Island Glacier spanning the LGM and Holocene periods is derived from spatially extensive IRHs. The connection between RES profiles and the WAIS Divide ice core enables the direct dating of the IRHs, and reveals that they match large peaks in sulphate concentrations which are unparalleled in the 68,000 year-old record, thus suggesting that the cause of these IRHs ... Doctoral or Postdoctoral Thesis Antarc* Antarctic Antarctica ice core Ice Sheet Pine Island Pine Island Glacier The Cryosphere Thwaites Glacier West Antarctica Edinburgh Research Archive (ERA - University of Edinburgh) Antarctic The Antarctic West Antarctica Pine Island Glacier ENVELOPE(-101.000,-101.000,-75.000,-75.000) Thwaites Glacier ENVELOPE(-106.750,-106.750,-75.500,-75.500) |