Reconstructing spatially variable mass balances from past ice extents by inverse modeling

ABSTRACT With the conclusion of the Last Glacial Maximum (LGM), about 20 000 years ago, ended the most recent long-lasting cold phase in Earth history. This last glacial advance left a strong observable imprint on the landscape, such as moraines, trimlines and other glacial geomorphic features. Thes...

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Published in:Journal of Glaciology
Main Authors: VIŠNJEVIĆ, VJERAN, HERMAN, FRÉDÉRIC, PODLADCHIKOV, YURY
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2018
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2018.82
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143018000825
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spelling crcambridgeupr:10.1017/jog.2018.82 2024-03-03T08:46:00+00:00 Reconstructing spatially variable mass balances from past ice extents by inverse modeling VIŠNJEVIĆ, VJERAN HERMAN, FRÉDÉRIC PODLADCHIKOV, YURY 2018 http://dx.doi.org/10.1017/jog.2018.82 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143018000825 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 64, issue 248, page 957-968 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 2018 crcambridgeupr https://doi.org/10.1017/jog.2018.82 2024-02-08T08:43:51Z ABSTRACT With the conclusion of the Last Glacial Maximum (LGM), about 20 000 years ago, ended the most recent long-lasting cold phase in Earth history. This last glacial advance left a strong observable imprint on the landscape, such as moraines, trimlines and other glacial geomorphic features. These features reflect the extent of former glaciers and ice caps, which in turn provides information on past temperature and precipitation conditions. Here we present an inverse approach to reconstruct the equilibrium line altitudes ( E ) from observed ice extents. The ice-flow model is developed solving the mass conservation equation using the shallow ice approximation and implemented using Graphical Processing Units (GPUs). We present the theoretical basis of the inversion method, which relies on a Tikhonov regularization, and demonstrate its ability to constrain spatial variations in mass balance with idealized and real glaciers. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 64 248 957 968
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
VIŠNJEVIĆ, VJERAN
HERMAN, FRÉDÉRIC
PODLADCHIKOV, YURY
Reconstructing spatially variable mass balances from past ice extents by inverse modeling
topic_facet Earth-Surface Processes
description ABSTRACT With the conclusion of the Last Glacial Maximum (LGM), about 20 000 years ago, ended the most recent long-lasting cold phase in Earth history. This last glacial advance left a strong observable imprint on the landscape, such as moraines, trimlines and other glacial geomorphic features. These features reflect the extent of former glaciers and ice caps, which in turn provides information on past temperature and precipitation conditions. Here we present an inverse approach to reconstruct the equilibrium line altitudes ( E ) from observed ice extents. The ice-flow model is developed solving the mass conservation equation using the shallow ice approximation and implemented using Graphical Processing Units (GPUs). We present the theoretical basis of the inversion method, which relies on a Tikhonov regularization, and demonstrate its ability to constrain spatial variations in mass balance with idealized and real glaciers.
format Article in Journal/Newspaper
author VIŠNJEVIĆ, VJERAN
HERMAN, FRÉDÉRIC
PODLADCHIKOV, YURY
author_facet VIŠNJEVIĆ, VJERAN
HERMAN, FRÉDÉRIC
PODLADCHIKOV, YURY
author_sort VIŠNJEVIĆ, VJERAN
title Reconstructing spatially variable mass balances from past ice extents by inverse modeling
title_short Reconstructing spatially variable mass balances from past ice extents by inverse modeling
title_full Reconstructing spatially variable mass balances from past ice extents by inverse modeling
title_fullStr Reconstructing spatially variable mass balances from past ice extents by inverse modeling
title_full_unstemmed Reconstructing spatially variable mass balances from past ice extents by inverse modeling
title_sort reconstructing spatially variable mass balances from past ice extents by inverse modeling
publisher Cambridge University Press (CUP)
publishDate 2018
url http://dx.doi.org/10.1017/jog.2018.82
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143018000825
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 64, issue 248, page 957-968
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2018.82
container_title Journal of Glaciology
container_volume 64
container_issue 248
container_start_page 957
op_container_end_page 968
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