Numerical simulations of the (de)stabilization of the West Antarctic Ice Sheet ...

There is evidence that a self-sustaining ice discharge from the West Antarctic Ice Sheet (WAIS) has started, potentially leading to its disintegration. The associated sea level rise of more than 3m would pose a serious challenge to highly populated areas including metropolises such as Calcutta, Shan...

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Main Authors: Feldmann, Johannes, Levermann, Anders, Mengel, Matthias
Format: Dataset
Language:English
Published: PANGAEA 2019
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.907702
https://doi.pangaea.de/10.1594/PANGAEA.907702
id ftdatacite:10.1594/pangaea.907702
record_format openpolar
spelling ftdatacite:10.1594/pangaea.907702 2024-09-15T17:47:31+00:00 Numerical simulations of the (de)stabilization of the West Antarctic Ice Sheet ... Feldmann, Johannes Levermann, Anders Mengel, Matthias 2019 application/zip https://dx.doi.org/10.1594/pangaea.907702 https://doi.pangaea.de/10.1594/PANGAEA.907702 en eng PANGAEA https://dx.doi.org/10.1126/sciadv.aaw4132 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 instability numerical modeling West Antarctic Ice Sheet Multiple investigations Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 dataset Supplementary Dataset Dataset 2019 ftdatacite https://doi.org/10.1594/pangaea.90770210.1126/sciadv.aaw4132 2024-08-01T10:54:23Z There is evidence that a self-sustaining ice discharge from the West Antarctic Ice Sheet (WAIS) has started, potentially leading to its disintegration. The associated sea level rise of more than 3m would pose a serious challenge to highly populated areas including metropolises such as Calcutta, Shanghai, New York City, and Tokyo. Here, we show that the WAIS may be stabilized through mass deposition in coastal regions around Pine Island and Thwaites glaciers. In our numerical simulations, a minimum of 7400 Gt of additional snowfall stabilizes the flow if applied over a short period of 10 years onto the region (−2 mm year−1 sea level equivalent). Mass deposition at a lower rate increases the intervention time and the required total amount of snow. We find that the precise conditions of such an operation are crucial, and potential benefits need to be weighed against environmental hazards, future risks, and enormous technical challenges. ... : Snapshots for a set of three simulations (shown in Figs. 2 and 3 of the paper)Forcing_8000Gt_20yr --> forcing with 8000 Gt of additional snow over 20 yrForcing_8000Gt_40yr --> forcing with 8000 Gt of additional snow over 40 yrNoForcing_Reference --> no addition of snow ... Dataset Antarc* Antarctic Ice Sheet Sea ice DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic instability
numerical modeling
West Antarctic Ice Sheet
Multiple investigations
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158
spellingShingle instability
numerical modeling
West Antarctic Ice Sheet
Multiple investigations
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158
Feldmann, Johannes
Levermann, Anders
Mengel, Matthias
Numerical simulations of the (de)stabilization of the West Antarctic Ice Sheet ...
topic_facet instability
numerical modeling
West Antarctic Ice Sheet
Multiple investigations
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158
description There is evidence that a self-sustaining ice discharge from the West Antarctic Ice Sheet (WAIS) has started, potentially leading to its disintegration. The associated sea level rise of more than 3m would pose a serious challenge to highly populated areas including metropolises such as Calcutta, Shanghai, New York City, and Tokyo. Here, we show that the WAIS may be stabilized through mass deposition in coastal regions around Pine Island and Thwaites glaciers. In our numerical simulations, a minimum of 7400 Gt of additional snowfall stabilizes the flow if applied over a short period of 10 years onto the region (−2 mm year−1 sea level equivalent). Mass deposition at a lower rate increases the intervention time and the required total amount of snow. We find that the precise conditions of such an operation are crucial, and potential benefits need to be weighed against environmental hazards, future risks, and enormous technical challenges. ... : Snapshots for a set of three simulations (shown in Figs. 2 and 3 of the paper)Forcing_8000Gt_20yr --> forcing with 8000 Gt of additional snow over 20 yrForcing_8000Gt_40yr --> forcing with 8000 Gt of additional snow over 40 yrNoForcing_Reference --> no addition of snow ...
format Dataset
author Feldmann, Johannes
Levermann, Anders
Mengel, Matthias
author_facet Feldmann, Johannes
Levermann, Anders
Mengel, Matthias
author_sort Feldmann, Johannes
title Numerical simulations of the (de)stabilization of the West Antarctic Ice Sheet ...
title_short Numerical simulations of the (de)stabilization of the West Antarctic Ice Sheet ...
title_full Numerical simulations of the (de)stabilization of the West Antarctic Ice Sheet ...
title_fullStr Numerical simulations of the (de)stabilization of the West Antarctic Ice Sheet ...
title_full_unstemmed Numerical simulations of the (de)stabilization of the West Antarctic Ice Sheet ...
title_sort numerical simulations of the (de)stabilization of the west antarctic ice sheet ...
publisher PANGAEA
publishDate 2019
url https://dx.doi.org/10.1594/pangaea.907702
https://doi.pangaea.de/10.1594/PANGAEA.907702
genre Antarc*
Antarctic
Ice Sheet
Sea ice
genre_facet Antarc*
Antarctic
Ice Sheet
Sea ice
op_relation https://dx.doi.org/10.1126/sciadv.aaw4132
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.90770210.1126/sciadv.aaw4132
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