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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Main Author: Feldmann, Johannes
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.946709
https://doi.org/10.1594/PANGAEA.946709
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.946709
record_format openpolar
spelling 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
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