Ice thickness and volume of the Renland Ice Cap, East Greenland
Abstract To assess the amount of ice volume stored in glaciers or ice caps, a method to estimate ice thickness distribution is required for glaciers where no direct observations are available. In this study, we use an existing inverse method to estimate the bedrock topography and ice thickness of th...
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Cambridge University Press (CUP)
2021
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Online Access: | http://dx.doi.org/10.1017/jog.2021.11 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143021000113 |
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crcambridgeupr:10.1017/jog.2021.11 2024-03-03T08:43:59+00:00 Ice thickness and volume of the Renland Ice Cap, East Greenland Koldtoft, Iben Grinsted, Aslak Vinther, Bo M. Hvidberg, Christine S. 2021 http://dx.doi.org/10.1017/jog.2021.11 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143021000113 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology page 1-13 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 2021 crcambridgeupr https://doi.org/10.1017/jog.2021.11 2024-02-08T08:29:20Z Abstract To assess the amount of ice volume stored in glaciers or ice caps, a method to estimate ice thickness distribution is required for glaciers where no direct observations are available. In this study, we use an existing inverse method to estimate the bedrock topography and ice thickness of the Renland Ice Cap, East Greenland, using satellite-based observations of the surface topography. The inverse approach involves a procedure in which an ice dynamical model is used to build-up an ice cap in steady state with climate forcing from a regional climate model, and the bedrock is iteratively adjusted until the modelled and observed surface topography match. We validate our model results against information from airborne radar data and satellite observed surface velocity, and we find that the inferred ice thickness and thereby the stored total volume of the ice cap is sensitive to the assumed ice softness and basal slipperiness. The best basal model parameters for the Renland Ice Cap are determined and the best estimated total ice volume of 384 km 3 is found. The Renland Ice Cap is particularly interesting because of its location at a high elevation plateau and hence assumed low sensitivity to climate change. Article in Journal/Newspaper East Greenland Greenland Ice cap Journal of Glaciology Cambridge University Press Greenland Renland ENVELOPE(-26.750,-26.750,71.200,71.200) Journal of Glaciology 67 264 714 726 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Koldtoft, Iben Grinsted, Aslak Vinther, Bo M. Hvidberg, Christine S. Ice thickness and volume of the Renland Ice Cap, East Greenland |
topic_facet |
Earth-Surface Processes |
description |
Abstract To assess the amount of ice volume stored in glaciers or ice caps, a method to estimate ice thickness distribution is required for glaciers where no direct observations are available. In this study, we use an existing inverse method to estimate the bedrock topography and ice thickness of the Renland Ice Cap, East Greenland, using satellite-based observations of the surface topography. The inverse approach involves a procedure in which an ice dynamical model is used to build-up an ice cap in steady state with climate forcing from a regional climate model, and the bedrock is iteratively adjusted until the modelled and observed surface topography match. We validate our model results against information from airborne radar data and satellite observed surface velocity, and we find that the inferred ice thickness and thereby the stored total volume of the ice cap is sensitive to the assumed ice softness and basal slipperiness. The best basal model parameters for the Renland Ice Cap are determined and the best estimated total ice volume of 384 km 3 is found. The Renland Ice Cap is particularly interesting because of its location at a high elevation plateau and hence assumed low sensitivity to climate change. |
format |
Article in Journal/Newspaper |
author |
Koldtoft, Iben Grinsted, Aslak Vinther, Bo M. Hvidberg, Christine S. |
author_facet |
Koldtoft, Iben Grinsted, Aslak Vinther, Bo M. Hvidberg, Christine S. |
author_sort |
Koldtoft, Iben |
title |
Ice thickness and volume of the Renland Ice Cap, East Greenland |
title_short |
Ice thickness and volume of the Renland Ice Cap, East Greenland |
title_full |
Ice thickness and volume of the Renland Ice Cap, East Greenland |
title_fullStr |
Ice thickness and volume of the Renland Ice Cap, East Greenland |
title_full_unstemmed |
Ice thickness and volume of the Renland Ice Cap, East Greenland |
title_sort |
ice thickness and volume of the renland ice cap, east greenland |
publisher |
Cambridge University Press (CUP) |
publishDate |
2021 |
url |
http://dx.doi.org/10.1017/jog.2021.11 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143021000113 |
long_lat |
ENVELOPE(-26.750,-26.750,71.200,71.200) |
geographic |
Greenland Renland |
geographic_facet |
Greenland Renland |
genre |
East Greenland Greenland Ice cap Journal of Glaciology |
genre_facet |
East Greenland Greenland Ice cap Journal of Glaciology |
op_source |
Journal of Glaciology page 1-13 ISSN 0022-1430 1727-5652 |
op_rights |
http://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.1017/jog.2021.11 |
container_title |
Journal of Glaciology |
container_volume |
67 |
container_issue |
264 |
container_start_page |
714 |
op_container_end_page |
726 |
_version_ |
1792499466435035136 |