Investigating marine-terminating glacier behaviour in Greenland
Recent changes at marine-terminating glaciers in Greenland have suggested a dynamic and sensitive response to climate via atmospheric and oceanic warming. Ice loss from marine-terminating glaciers has already contributed significantly to global sea level rise and this is likely to continue with futu...
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The University of Edinburgh
2022
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ftunivedinburgh:oai:era.ed.ac.uk:1842/38616 2023-07-30T04:03:36+02:00 Investigating marine-terminating glacier behaviour in Greenland Bunce, Charlotte Nienow, Peter Gourmelen, Noel Newton, Anthony Natural Environment Research Council (NERC) 2022-02-23 application/pdf https://hdl.handle.net/1842/38616 https://doi.org/10.7488/era/1879 en eng The University of Edinburgh Bunce, C., J. R. Carr, P. W. Nienow, N. Ross, and R. Killick (2018). “Ice front change of marine-terminating outlet glaciers in northwest and southeast Greenland during the 21st century”. In: Journal of Glaciology 64.246, pp. 523–535. doi:10.1017/ jog.2018.44 Bunce, C., P. Nienow, A. Sole, T. Cowton, and B. Davison (2021). “Influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large Greenlandic tidewater glacier”. In: Journal of Glaciology 67.262, pp. 343–352. doi: 10. 1017/jog.2020.109 Bunce, C. (2016). Contrasting the Dynamic Response of Marine-Terminating Outlet Glaciers in North-West and South-East Greenland to 21st Century Climate Warming. MPhil Thesis, Newcastle Universit https://hdl.handle.net/1842/38616 http://dx.doi.org/10.7488/era/1879 Greenland ice sheet glaciology ice-ocean interaction climate change Thesis or Dissertation Doctoral PhD Doctor of Philosophy 2022 ftunivedinburgh https://doi.org/10.7488/era/1879 2023-07-09T20:30:06Z Recent changes at marine-terminating glaciers in Greenland have suggested a dynamic and sensitive response to climate via atmospheric and oceanic warming. Ice loss from marine-terminating glaciers has already contributed significantly to global sea level rise and this is likely to continue with future warming. However, understanding the processes connecting this warming to ice loss from marine-terminating glaciers remains confounded. This is in part due to the complex and dynamic interactions between various potential forcing mechanisms and also due to limited observations of marine-terminating glacier behaviour at sufficiently high spatial and temporal resolutions. This thesis combines remote sensing techniques and field-based observations to investigate ice loss at marine-terminating glaciers at a range of spatial and temporal scales. Here, the overarching aim is to better elucidate the dominant controls on ice loss at marine-terminating glaciers and thus the role they play in the sensitivity of the Greenland Ice Sheet to future environmental change. This thesis first aimed to address one of the primary gaps in observations regarding how key regions of the ice sheet have responded to environmental change, by deriving a detailed record of marine-terminating glacier terminus positions in southeast and northwest Greenland between 2000 and 2015. Through analysing these two key regions of ice loss alongside potential controls on retreat, the ambition was to better constrain the mechanisms driving region-wide change. The results revealed that irrespective of individual spatial or temporal variations in glacier terminus behaviour within or between these two regions, there was an overriding signal of marine-terminating glacier retreat (and thus ice loss) during the 21st Century. Overall, 97% of glaciers experienced terminus retreat, with mean annual retreat rates of -90 m a−1 and -70 m a−1 in the northwest and south-east respectively. This work also showed that changes in bed and fjord geometry were key controls on ... Doctoral or Postdoctoral Thesis glacier Greenland Ice Sheet Journal of Glaciology Edinburgh Research Archive (ERA - University of Edinburgh) Greenland |
institution |
Open Polar |
collection |
Edinburgh Research Archive (ERA - University of Edinburgh) |
op_collection_id |
ftunivedinburgh |
language |
English |
topic |
Greenland ice sheet glaciology ice-ocean interaction climate change |
spellingShingle |
Greenland ice sheet glaciology ice-ocean interaction climate change Bunce, Charlotte Investigating marine-terminating glacier behaviour in Greenland |
topic_facet |
Greenland ice sheet glaciology ice-ocean interaction climate change |
description |
Recent changes at marine-terminating glaciers in Greenland have suggested a dynamic and sensitive response to climate via atmospheric and oceanic warming. Ice loss from marine-terminating glaciers has already contributed significantly to global sea level rise and this is likely to continue with future warming. However, understanding the processes connecting this warming to ice loss from marine-terminating glaciers remains confounded. This is in part due to the complex and dynamic interactions between various potential forcing mechanisms and also due to limited observations of marine-terminating glacier behaviour at sufficiently high spatial and temporal resolutions. This thesis combines remote sensing techniques and field-based observations to investigate ice loss at marine-terminating glaciers at a range of spatial and temporal scales. Here, the overarching aim is to better elucidate the dominant controls on ice loss at marine-terminating glaciers and thus the role they play in the sensitivity of the Greenland Ice Sheet to future environmental change. This thesis first aimed to address one of the primary gaps in observations regarding how key regions of the ice sheet have responded to environmental change, by deriving a detailed record of marine-terminating glacier terminus positions in southeast and northwest Greenland between 2000 and 2015. Through analysing these two key regions of ice loss alongside potential controls on retreat, the ambition was to better constrain the mechanisms driving region-wide change. The results revealed that irrespective of individual spatial or temporal variations in glacier terminus behaviour within or between these two regions, there was an overriding signal of marine-terminating glacier retreat (and thus ice loss) during the 21st Century. Overall, 97% of glaciers experienced terminus retreat, with mean annual retreat rates of -90 m a−1 and -70 m a−1 in the northwest and south-east respectively. This work also showed that changes in bed and fjord geometry were key controls on ... |
author2 |
Nienow, Peter Gourmelen, Noel Newton, Anthony Natural Environment Research Council (NERC) |
format |
Doctoral or Postdoctoral Thesis |
author |
Bunce, Charlotte |
author_facet |
Bunce, Charlotte |
author_sort |
Bunce, Charlotte |
title |
Investigating marine-terminating glacier behaviour in Greenland |
title_short |
Investigating marine-terminating glacier behaviour in Greenland |
title_full |
Investigating marine-terminating glacier behaviour in Greenland |
title_fullStr |
Investigating marine-terminating glacier behaviour in Greenland |
title_full_unstemmed |
Investigating marine-terminating glacier behaviour in Greenland |
title_sort |
investigating marine-terminating glacier behaviour in greenland |
publisher |
The University of Edinburgh |
publishDate |
2022 |
url |
https://hdl.handle.net/1842/38616 https://doi.org/10.7488/era/1879 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
glacier Greenland Ice Sheet Journal of Glaciology |
genre_facet |
glacier Greenland Ice Sheet Journal of Glaciology |
op_relation |
Bunce, C., J. R. Carr, P. W. Nienow, N. Ross, and R. Killick (2018). “Ice front change of marine-terminating outlet glaciers in northwest and southeast Greenland during the 21st century”. In: Journal of Glaciology 64.246, pp. 523–535. doi:10.1017/ jog.2018.44 Bunce, C., P. Nienow, A. Sole, T. Cowton, and B. Davison (2021). “Influence of glacier runoff and near-terminus subglacial hydrology on frontal ablation at a large Greenlandic tidewater glacier”. In: Journal of Glaciology 67.262, pp. 343–352. doi: 10. 1017/jog.2020.109 Bunce, C. (2016). Contrasting the Dynamic Response of Marine-Terminating Outlet Glaciers in North-West and South-East Greenland to 21st Century Climate Warming. MPhil Thesis, Newcastle Universit https://hdl.handle.net/1842/38616 http://dx.doi.org/10.7488/era/1879 |
op_doi |
https://doi.org/10.7488/era/1879 |
_version_ |
1772814634260103168 |