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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Published in:Journal of Glaciology
Main Authors: Koldtoft, Iben, Grinsted, Aslak, Vinther, Bo M., Hvidberg, Christine S.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2021
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2021.11
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143021000113
id crcambridgeupr:10.1017/jog.2021.11
record_format openpolar
spelling 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
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