Evolution of high-Arctic glacial landforms during deglaciation
Glacial landsystems in the high-Arctic have been reported to undergo geomorphological transformation during deglaciation. This research evaluates moraine evolution over a decadal timescale at Midtre Lovénbreen, Svalbard. This work is of interest because glacial landforms developed in Svalbard have b...
Published in: | Geomorphology |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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2018
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Online Access: | https://discovery.dundee.ac.uk/en/publications/0d14b26f-006f-4b9d-8824-57adf2261420 https://doi.org/10.1016/j.geomorph.2018.03.027 https://discovery.dundee.ac.uk/ws/files/20675402/1_s2.0_S0169555X18301387_main.pdf |
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ftunivdundeepure:oai:discovery.dundee.ac.uk:publications/0d14b26f-006f-4b9d-8824-57adf2261420 2024-09-15T17:50:34+00:00 Evolution of high-Arctic glacial landforms during deglaciation Midgley, N. G. Tonkin, T. N. Graham, D. J. Cook, S. J. 2018-06-15 application/pdf https://discovery.dundee.ac.uk/en/publications/0d14b26f-006f-4b9d-8824-57adf2261420 https://doi.org/10.1016/j.geomorph.2018.03.027 https://discovery.dundee.ac.uk/ws/files/20675402/1_s2.0_S0169555X18301387_main.pdf eng eng https://discovery.dundee.ac.uk/en/publications/0d14b26f-006f-4b9d-8824-57adf2261420 info:eu-repo/semantics/openAccess Midgley , N G , Tonkin , T N , Graham , D J & Cook , S J 2018 , ' Evolution of high-Arctic glacial landforms during deglaciation ' , Geomorphology , vol. 311 , pp. 63-75 . https://doi.org/10.1016/j.geomorph.2018.03.027 Ground penetrating radar (GPR) Ice-cored moraine Midtre Lovénbreen Svalbard Structure-from-motion (SfM) Unmanned aerial vehicle (UAV) /dk/atira/pure/subjectarea/asjc/1900/1904 name=Earth-Surface Processes article 2018 ftunivdundeepure https://doi.org/10.1016/j.geomorph.2018.03.027 2024-07-09T14:14:10Z Glacial landsystems in the high-Arctic have been reported to undergo geomorphological transformation during deglaciation. This research evaluates moraine evolution over a decadal timescale at Midtre Lovénbreen, Svalbard. This work is of interest because glacial landforms developed in Svalbard have been used as an analogue for landforms developed during Pleistocene mid-latitude glaciation. Ground penetrating radar was used to investigate the subsurface characteristics of moraines. To determine surface change, a LiDAR topographic data set (obtained 2003) and a UAV-derived (obtained 2014) digital surface model processed using structure-from-motion (SfM) are also compared. Evaluation of these data sets together enables subsurface character and landform response to climatic amelioration to be linked. Ground penetrating radar evidence shows that the moraine substrate at Midtre Lovénbreen includes ice-rich (radar velocities of 0.17 m ns −1 ) and debris-rich (radar velocities of 0.1–0.13 m ns −1 ) zones. The ice-rich zones are demonstrated to exhibit relatively high rates of surface change (mean thresholded rate of −4.39 m over the 11-year observation period). However, the debris-rich zones show a relatively low rate of surface change (mean thresholded rate of −0.98 m over the 11-year observation period), and the morphology of the debris-rich landforms appear stable over the observation period. A complex response of proglacial landforms to climatic warming is shown to occur within and between glacier forelands as indicated by spatially variable surface lowering rates. Landform response is controlled by the ice-debris balance of the moraine substrate, along with the topographic context (such as the influence of meltwater). Site-specific characteristics such as surface debris thickness and glaciofluvial drainage are, therefore, argued to be a highly important control on surface evolution in ice-cored terrain, resulting in a diverse response of high-Arctic glacial landsystems to climatic amelioration. These results ... Article in Journal/Newspaper Arctic glacier Svalbard Discovery - University of Dundee Online Publications Geomorphology 311 63 75 |
institution |
Open Polar |
collection |
Discovery - University of Dundee Online Publications |
op_collection_id |
ftunivdundeepure |
language |
English |
topic |
Ground penetrating radar (GPR) Ice-cored moraine Midtre Lovénbreen Svalbard Structure-from-motion (SfM) Unmanned aerial vehicle (UAV) /dk/atira/pure/subjectarea/asjc/1900/1904 name=Earth-Surface Processes |
spellingShingle |
Ground penetrating radar (GPR) Ice-cored moraine Midtre Lovénbreen Svalbard Structure-from-motion (SfM) Unmanned aerial vehicle (UAV) /dk/atira/pure/subjectarea/asjc/1900/1904 name=Earth-Surface Processes Midgley, N. G. Tonkin, T. N. Graham, D. J. Cook, S. J. Evolution of high-Arctic glacial landforms during deglaciation |
topic_facet |
Ground penetrating radar (GPR) Ice-cored moraine Midtre Lovénbreen Svalbard Structure-from-motion (SfM) Unmanned aerial vehicle (UAV) /dk/atira/pure/subjectarea/asjc/1900/1904 name=Earth-Surface Processes |
description |
Glacial landsystems in the high-Arctic have been reported to undergo geomorphological transformation during deglaciation. This research evaluates moraine evolution over a decadal timescale at Midtre Lovénbreen, Svalbard. This work is of interest because glacial landforms developed in Svalbard have been used as an analogue for landforms developed during Pleistocene mid-latitude glaciation. Ground penetrating radar was used to investigate the subsurface characteristics of moraines. To determine surface change, a LiDAR topographic data set (obtained 2003) and a UAV-derived (obtained 2014) digital surface model processed using structure-from-motion (SfM) are also compared. Evaluation of these data sets together enables subsurface character and landform response to climatic amelioration to be linked. Ground penetrating radar evidence shows that the moraine substrate at Midtre Lovénbreen includes ice-rich (radar velocities of 0.17 m ns −1 ) and debris-rich (radar velocities of 0.1–0.13 m ns −1 ) zones. The ice-rich zones are demonstrated to exhibit relatively high rates of surface change (mean thresholded rate of −4.39 m over the 11-year observation period). However, the debris-rich zones show a relatively low rate of surface change (mean thresholded rate of −0.98 m over the 11-year observation period), and the morphology of the debris-rich landforms appear stable over the observation period. A complex response of proglacial landforms to climatic warming is shown to occur within and between glacier forelands as indicated by spatially variable surface lowering rates. Landform response is controlled by the ice-debris balance of the moraine substrate, along with the topographic context (such as the influence of meltwater). Site-specific characteristics such as surface debris thickness and glaciofluvial drainage are, therefore, argued to be a highly important control on surface evolution in ice-cored terrain, resulting in a diverse response of high-Arctic glacial landsystems to climatic amelioration. These results ... |
format |
Article in Journal/Newspaper |
author |
Midgley, N. G. Tonkin, T. N. Graham, D. J. Cook, S. J. |
author_facet |
Midgley, N. G. Tonkin, T. N. Graham, D. J. Cook, S. J. |
author_sort |
Midgley, N. G. |
title |
Evolution of high-Arctic glacial landforms during deglaciation |
title_short |
Evolution of high-Arctic glacial landforms during deglaciation |
title_full |
Evolution of high-Arctic glacial landforms during deglaciation |
title_fullStr |
Evolution of high-Arctic glacial landforms during deglaciation |
title_full_unstemmed |
Evolution of high-Arctic glacial landforms during deglaciation |
title_sort |
evolution of high-arctic glacial landforms during deglaciation |
publishDate |
2018 |
url |
https://discovery.dundee.ac.uk/en/publications/0d14b26f-006f-4b9d-8824-57adf2261420 https://doi.org/10.1016/j.geomorph.2018.03.027 https://discovery.dundee.ac.uk/ws/files/20675402/1_s2.0_S0169555X18301387_main.pdf |
genre |
Arctic glacier Svalbard |
genre_facet |
Arctic glacier Svalbard |
op_source |
Midgley , N G , Tonkin , T N , Graham , D J & Cook , S J 2018 , ' Evolution of high-Arctic glacial landforms during deglaciation ' , Geomorphology , vol. 311 , pp. 63-75 . https://doi.org/10.1016/j.geomorph.2018.03.027 |
op_relation |
https://discovery.dundee.ac.uk/en/publications/0d14b26f-006f-4b9d-8824-57adf2261420 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1016/j.geomorph.2018.03.027 |
container_title |
Geomorphology |
container_volume |
311 |
container_start_page |
63 |
op_container_end_page |
75 |
_version_ |
1810292383391154176 |