PISM simulations of idealized shear-margin vs. ice-stream melt
PISM model output, runs scripts and plotting scripts. The idealized simulations investigate the influence of basal melting in two different ice-shelf regions on the time-dependent response of an isothermal, inherently buttressed ice-sheet-shelf system. The basal-melt perturbations are applied close...
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.946709 https://doi.org/10.1594/PANGAEA.946709 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.946709 2024-10-13T14:03:25+00:00 PISM simulations of idealized shear-margin vs. ice-stream melt Feldmann, Johannes 2022 application/zip, 3.6 GBytes https://doi.pangaea.de/10.1594/PANGAEA.946709 https://doi.org/10.1594/PANGAEA.946709 en eng PANGAEA Feldmann, Johannes; Reese, Ronja; Winkelmann, Ricarda; Levermann, Anders (2022): Shear-margin melting causes stronger transient ice discharge than ice-stream melting in idealized simulations. The Cryosphere, 16(5), 1927-1940, https://doi.org/10.5194/tc-16-1927-2022 https://doi.pangaea.de/10.1594/PANGAEA.946709 https://doi.org/10.1594/PANGAEA.946709 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Antarctic Ice Sheet glacier Ice Sheet Modelling ice shelf basal melting Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas sea level change SPP1158 SPP 1158 dataset 2022 ftpangaea https://doi.org/10.1594/PANGAEA.94670910.5194/tc-16-1927-2022 2024-10-02T00:42:44Z PISM model output, runs scripts and plotting scripts. The idealized simulations investigate the influence of basal melting in two different ice-shelf regions on the time-dependent response of an isothermal, inherently buttressed ice-sheet-shelf system. The basal-melt perturbations are applied close to the grounding line in the ice-shelf's 1) ice-stream region, where the ice shelf is fed by the fastest ice masses that stream through the upstream bed trough and 2) shear margins, where the ice flow is slower. Dataset Antarc* Antarctic Arctic Ice Sheet Ice Shelf Sea ice The Cryosphere PANGAEA - Data Publisher for Earth & Environmental Science Arctic Antarctic |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Antarctic Ice Sheet glacier Ice Sheet Modelling ice shelf basal melting Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas sea level change SPP1158 SPP 1158 |
spellingShingle |
Antarctic Ice Sheet glacier Ice Sheet Modelling ice shelf basal melting Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas sea level change SPP1158 SPP 1158 Feldmann, Johannes PISM simulations of idealized shear-margin vs. ice-stream melt |
topic_facet |
Antarctic Ice Sheet glacier Ice Sheet Modelling ice shelf basal melting Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas sea level change SPP1158 SPP 1158 |
description |
PISM model output, runs scripts and plotting scripts. The idealized simulations investigate the influence of basal melting in two different ice-shelf regions on the time-dependent response of an isothermal, inherently buttressed ice-sheet-shelf system. The basal-melt perturbations are applied close to the grounding line in the ice-shelf's 1) ice-stream region, where the ice shelf is fed by the fastest ice masses that stream through the upstream bed trough and 2) shear margins, where the ice flow is slower. |
format |
Dataset |
author |
Feldmann, Johannes |
author_facet |
Feldmann, Johannes |
author_sort |
Feldmann, Johannes |
title |
PISM simulations of idealized shear-margin vs. ice-stream melt |
title_short |
PISM simulations of idealized shear-margin vs. ice-stream melt |
title_full |
PISM simulations of idealized shear-margin vs. ice-stream melt |
title_fullStr |
PISM simulations of idealized shear-margin vs. ice-stream melt |
title_full_unstemmed |
PISM simulations of idealized shear-margin vs. ice-stream melt |
title_sort |
pism simulations of idealized shear-margin vs. ice-stream melt |
publisher |
PANGAEA |
publishDate |
2022 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.946709 https://doi.org/10.1594/PANGAEA.946709 |
geographic |
Arctic Antarctic |
geographic_facet |
Arctic Antarctic |
genre |
Antarc* Antarctic Arctic Ice Sheet Ice Shelf Sea ice The Cryosphere |
genre_facet |
Antarc* Antarctic Arctic Ice Sheet Ice Shelf Sea ice The Cryosphere |
op_relation |
Feldmann, Johannes; Reese, Ronja; Winkelmann, Ricarda; Levermann, Anders (2022): Shear-margin melting causes stronger transient ice discharge than ice-stream melting in idealized simulations. The Cryosphere, 16(5), 1927-1940, https://doi.org/10.5194/tc-16-1927-2022 https://doi.pangaea.de/10.1594/PANGAEA.946709 https://doi.org/10.1594/PANGAEA.946709 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.94670910.5194/tc-16-1927-2022 |
_version_ |
1812808398709719040 |