Nature and dynamics of ice-stream beds: assessing their role in ice-sheet stability
Ice streams are fast flowing outlet glaciers through which over 90% of the ice stored within the Antarctic Ice Sheet drains. The dynamic behaviour of ice streams is therefore crucial in controlling the mass balance of the ice sheet. Over the past few decades, Antarctica has been losing mass. Much of...
Published in: | Nature Communications |
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Main Author: | |
Other Authors: | , , |
Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
Published: |
The University of Edinburgh
2018
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Subjects: | |
Online Access: | http://hdl.handle.net/1842/31399 |
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ftunivedinburgh:oai:era.ed.ac.uk:1842/31399 |
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openpolar |
institution |
Open Polar |
collection |
Edinburgh Research Archive (ERA - University of Edinburgh) |
op_collection_id |
ftunivedinburgh |
language |
English |
topic |
glaciology geophysics geomorphology radar Antarctica ice-sheet subglacial |
spellingShingle |
glaciology geophysics geomorphology radar Antarctica ice-sheet subglacial Davies, Damon Nature and dynamics of ice-stream beds: assessing their role in ice-sheet stability |
topic_facet |
glaciology geophysics geomorphology radar Antarctica ice-sheet subglacial |
description |
Ice streams are fast flowing outlet glaciers through which over 90% of the ice stored within the Antarctic Ice Sheet drains. The dynamic behaviour of ice streams is therefore crucial in controlling the mass balance of the ice sheet. Over the past few decades, Antarctica has been losing mass. Much of this mass loss has been focussed around coastal regions of the Antarctic Ice Sheet. Some of the most dramatic changes such as grounding-line retreat, acceleration and surface elevation change have been observed in Pine Island Glacier (PIG) and its neighbouring ice streams. This is of particular concern because these ice streams account for 10% of the discharge from the west Antarctic Ice Sheet and therefore have the potential to contribute significantly to global sea-level rise. One of the key challenges in accurately forecasting this future sea-level rise is improving understanding of processes occurring at the beds of ice streams. This requires detailed knowledge of the properties and dynamics of the bed. This thesis aims to address this knowledge gap by investigating the spatial and temporal characteristics of the bed of PIG using high-resolution geophysical data acquired in its trunk and tributaries and beneath the ice shelf. The thesis begins by analysing radar-derived high-resolution maps of subglacial topography. These data show a contrasting topography across the ice-bed interface. These diverse subglacial landscapes have an impact on ice flow through form drag, controlled by the size and orientation of bedrock undulations and protuberances. The next chapter provides a quantitative analysis of these landscapes using Fast Fourier analysis of subglacial roughness. This analysis investigates the roughness signature of subglacial bedforms and the how the orientation and wavelength of roughness elements determine their correlation with ice dynamic parameters. The slow-flowing inter-tributary site is found to have a distinct signature comparable to “ribbed” patterns of modelled basal shear stress and transverse ... |
author2 |
Bingham, Robert Hulton, Nick Natural Environment Research Council (NERC) |
format |
Doctoral or Postdoctoral Thesis |
author |
Davies, Damon |
author_facet |
Davies, Damon |
author_sort |
Davies, Damon |
title |
Nature and dynamics of ice-stream beds: assessing their role in ice-sheet stability |
title_short |
Nature and dynamics of ice-stream beds: assessing their role in ice-sheet stability |
title_full |
Nature and dynamics of ice-stream beds: assessing their role in ice-sheet stability |
title_fullStr |
Nature and dynamics of ice-stream beds: assessing their role in ice-sheet stability |
title_full_unstemmed |
Nature and dynamics of ice-stream beds: assessing their role in ice-sheet stability |
title_sort |
nature and dynamics of ice-stream beds: assessing their role in ice-sheet stability |
publisher |
The University of Edinburgh |
publishDate |
2018 |
url |
http://hdl.handle.net/1842/31399 |
long_lat |
ENVELOPE(-101.000,-101.000,-75.000,-75.000) |
geographic |
Antarctic Pine Island Glacier The Antarctic West Antarctic Ice Sheet |
geographic_facet |
Antarctic Pine Island Glacier The Antarctic West Antarctic Ice Sheet |
genre |
Antarc* Antarctic Antarctica Antarctica Journal Ice Sheet Ice Shelf Pine Island Pine Island Glacier The Cryosphere |
genre_facet |
Antarc* Antarctic Antarctica Antarctica Journal Ice Sheet Ice Shelf Pine Island Pine Island Glacier The Cryosphere |
op_relation |
The University of Edinburgh. College of Science and Engineering Bingham, R.G., Vaughan, D.G., King, E.C., Davies, D., Cornford, S.L., Smith, A.M., Arthern, R.J., Brisbourne, A.M., De Rydt, J., Graham, A.G., Spagnolo, M., Shean, D.E (2017). Diverse landscapes beneath Pine Island Glacier influence ice flow. Nature communications, 8(1), doi:10.1038/s41467-017-01597-y Davies, D., Bingham, R. G., King, E. C., Smith, A. M., Brisbourne, A. M., Spagnolo, M., Graham, A. G. C., Hogg, A. E., and Vaughan, D. G. (2017). How dynamic are ice-stream beds?, The Cryosphere, 12, pp.1615-1628 https://doi.org/10.5194/tc-12-1615-2018. Davies, D., Bingham, R.G., Graham, A.G.C., Spagnolo, M., Dutrieux, P., Vaughan, D.G., Jenkins, A. and Nitsche, F.O., (2017). High-resolution sub-ice-shelf seafloor records of twentieth century ungrounding and retreat of Pine Island Glacier, West Antarctica. Journal of Geophysical Research: Earth Surface, 122(9), pp.1698-1714. Brisbourne, A. M., A. M. Smith, D. G. Vaughan, E. C. King, D. Davies, R. G. Bingham, E. C. Smith, I. J. Nias, and S. H. R. Rosier (2017), Bed conditions of Pine Island Glacier, West Antarctica, Journal of Geophysical Research: Earth Surface, 122(1), 419–433, doi:10.1002/2016JF004033, 2016JF004033. http://hdl.handle.net/1842/31399 |
op_doi |
https://doi.org/10.1038/s41467-017-01597-y10.1002/2016JF004033 |
container_title |
Nature Communications |
container_volume |
8 |
container_issue |
1 |
_version_ |
1801383620089217024 |
spelling |
ftunivedinburgh:oai:era.ed.ac.uk:1842/31399 2024-06-09T07:40:08+00:00 Nature and dynamics of ice-stream beds: assessing their role in ice-sheet stability Davies, Damon Bingham, Robert Hulton, Nick Natural Environment Research Council (NERC) 03/07/2018 application/pdf http://hdl.handle.net/1842/31399 en eng The University of Edinburgh The University of Edinburgh. College of Science and Engineering Bingham, R.G., Vaughan, D.G., King, E.C., Davies, D., Cornford, S.L., Smith, A.M., Arthern, R.J., Brisbourne, A.M., De Rydt, J., Graham, A.G., Spagnolo, M., Shean, D.E (2017). Diverse landscapes beneath Pine Island Glacier influence ice flow. Nature communications, 8(1), doi:10.1038/s41467-017-01597-y Davies, D., Bingham, R. G., King, E. C., Smith, A. M., Brisbourne, A. M., Spagnolo, M., Graham, A. G. C., Hogg, A. E., and Vaughan, D. G. (2017). How dynamic are ice-stream beds?, The Cryosphere, 12, pp.1615-1628 https://doi.org/10.5194/tc-12-1615-2018. Davies, D., Bingham, R.G., Graham, A.G.C., Spagnolo, M., Dutrieux, P., Vaughan, D.G., Jenkins, A. and Nitsche, F.O., (2017). High-resolution sub-ice-shelf seafloor records of twentieth century ungrounding and retreat of Pine Island Glacier, West Antarctica. Journal of Geophysical Research: Earth Surface, 122(9), pp.1698-1714. Brisbourne, A. M., A. M. Smith, D. G. Vaughan, E. C. King, D. Davies, R. G. Bingham, E. C. Smith, I. J. Nias, and S. H. R. Rosier (2017), Bed conditions of Pine Island Glacier, West Antarctica, Journal of Geophysical Research: Earth Surface, 122(1), 419–433, doi:10.1002/2016JF004033, 2016JF004033. http://hdl.handle.net/1842/31399 glaciology geophysics geomorphology radar Antarctica ice-sheet subglacial Thesis or Dissertation Doctoral PhD Doctor of Philosophy 2018 ftunivedinburgh https://doi.org/10.1038/s41467-017-01597-y10.1002/2016JF004033 2024-05-10T03:12:17Z Ice streams are fast flowing outlet glaciers through which over 90% of the ice stored within the Antarctic Ice Sheet drains. The dynamic behaviour of ice streams is therefore crucial in controlling the mass balance of the ice sheet. Over the past few decades, Antarctica has been losing mass. Much of this mass loss has been focussed around coastal regions of the Antarctic Ice Sheet. Some of the most dramatic changes such as grounding-line retreat, acceleration and surface elevation change have been observed in Pine Island Glacier (PIG) and its neighbouring ice streams. This is of particular concern because these ice streams account for 10% of the discharge from the west Antarctic Ice Sheet and therefore have the potential to contribute significantly to global sea-level rise. One of the key challenges in accurately forecasting this future sea-level rise is improving understanding of processes occurring at the beds of ice streams. This requires detailed knowledge of the properties and dynamics of the bed. This thesis aims to address this knowledge gap by investigating the spatial and temporal characteristics of the bed of PIG using high-resolution geophysical data acquired in its trunk and tributaries and beneath the ice shelf. The thesis begins by analysing radar-derived high-resolution maps of subglacial topography. These data show a contrasting topography across the ice-bed interface. These diverse subglacial landscapes have an impact on ice flow through form drag, controlled by the size and orientation of bedrock undulations and protuberances. The next chapter provides a quantitative analysis of these landscapes using Fast Fourier analysis of subglacial roughness. This analysis investigates the roughness signature of subglacial bedforms and the how the orientation and wavelength of roughness elements determine their correlation with ice dynamic parameters. The slow-flowing inter-tributary site is found to have a distinct signature comparable to “ribbed” patterns of modelled basal shear stress and transverse ... Doctoral or Postdoctoral Thesis Antarc* Antarctic Antarctica Antarctica Journal Ice Sheet Ice Shelf Pine Island Pine Island Glacier The Cryosphere Edinburgh Research Archive (ERA - University of Edinburgh) Antarctic Pine Island Glacier ENVELOPE(-101.000,-101.000,-75.000,-75.000) The Antarctic West Antarctic Ice Sheet Nature Communications 8 1 |