Density matters: ice compressibility and glacier mass estimation

Ice flow models typically assume that ice is incompressible, a reasonable assumption because ice density changes are indeed small and have a correspondingly small effect on the overall mass balance of glaciers and ice sheets. Given the immense volume of the ice sheets, however, even relatively small...

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Published in:Journal of Glaciology
Main Author: Lipovsky, Bradley Paul
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2022
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2021.132
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143021001325
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spelling crcambridgeupr:10.1017/jog.2021.132 2024-03-03T08:45:25+00:00 Density matters: ice compressibility and glacier mass estimation Lipovsky, Bradley Paul 2022 http://dx.doi.org/10.1017/jog.2021.132 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143021001325 en eng Cambridge University Press (CUP) https://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 68, issue 270, page 831-832 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 2022 crcambridgeupr https://doi.org/10.1017/jog.2021.132 2024-02-08T08:30:27Z Ice flow models typically assume that ice is incompressible, a reasonable assumption because ice density changes are indeed small and have a correspondingly small effect on the overall mass balance of glaciers and ice sheets. Given the immense volume of the ice sheets, however, even relatively small changes may influence global mean sea level to a degree that severely impacts humanity (Hauer and others, 2020). Here, we quantify the role of gravitational compression and thermal contraction in estimating ice sheet mass. Article in Journal/Newspaper Ice Sheet Journal of Glaciology Cambridge University Press Journal of Glaciology 1 2
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Lipovsky, Bradley Paul
Density matters: ice compressibility and glacier mass estimation
topic_facet Earth-Surface Processes
description Ice flow models typically assume that ice is incompressible, a reasonable assumption because ice density changes are indeed small and have a correspondingly small effect on the overall mass balance of glaciers and ice sheets. Given the immense volume of the ice sheets, however, even relatively small changes may influence global mean sea level to a degree that severely impacts humanity (Hauer and others, 2020). Here, we quantify the role of gravitational compression and thermal contraction in estimating ice sheet mass.
format Article in Journal/Newspaper
author Lipovsky, Bradley Paul
author_facet Lipovsky, Bradley Paul
author_sort Lipovsky, Bradley Paul
title Density matters: ice compressibility and glacier mass estimation
title_short Density matters: ice compressibility and glacier mass estimation
title_full Density matters: ice compressibility and glacier mass estimation
title_fullStr Density matters: ice compressibility and glacier mass estimation
title_full_unstemmed Density matters: ice compressibility and glacier mass estimation
title_sort density matters: ice compressibility and glacier mass estimation
publisher Cambridge University Press (CUP)
publishDate 2022
url http://dx.doi.org/10.1017/jog.2021.132
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143021001325
genre Ice Sheet
Journal of Glaciology
genre_facet Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology
volume 68, issue 270, page 831-832
ISSN 0022-1430 1727-5652
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2021.132
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 2
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