Laurentide ice saddle mergers drive rapid sea level drops during glaciations

This is PISM v1.0 simulation data from a steady-state simulating the glaciation of Laurentide Ice Sheet by decreasing equilibrium-line altitude (ELA). We use a hybrid stress balance scheme in PISM (shallow ice approximation + shallow shelf approximation) and a thickness-based calving criterion. The...

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Bibliographic Details
Main Author: Weiwen Ji
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2021
Subjects:
Laurentide Ice Sheet
Ice Sheet
Online Access:https://doi.org/10.5281/zenodo.4751076
id ftzenodo:oai:zenodo.org:4751076
record_format openpolar
spelling ftzenodo:oai:zenodo.org:4751076 2024-09-15T18:12:11+00:00 Laurentide ice saddle mergers drive rapid sea level drops during glaciations Weiwen Ji 2021-05-12 https://doi.org/10.5281/zenodo.4751076 unknown Zenodo https://doi.org/10.5281/zenodo.4751075 https://doi.org/10.5281/zenodo.4751076 oai:zenodo.org:4751076 info:eu-repo/semantics/restrictedAccess Laurentide Ice Sheet info:eu-repo/semantics/other 2021 ftzenodo https://doi.org/10.5281/zenodo.475107610.5281/zenodo.4751075 2024-07-27T05:38:04Z This is PISM v1.0 simulation data from a steady-state simulating the glaciation of Laurentide Ice Sheet by decreasing equilibrium-line altitude (ELA). We use a hybrid stress balance scheme in PISM (shallow ice approximation + shallow shelf approximation) and a thickness-based calving criterion. The horizontal resolution is 20 km. it includes three ELA decreasing speeds (ELA gradually decreases in 20 kyr, 100kyr, and step changes). Other/Unknown Material Ice Sheet Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic Laurentide Ice Sheet
spellingShingle Laurentide Ice Sheet
Weiwen Ji
Laurentide ice saddle mergers drive rapid sea level drops during glaciations
topic_facet Laurentide Ice Sheet
description This is PISM v1.0 simulation data from a steady-state simulating the glaciation of Laurentide Ice Sheet by decreasing equilibrium-line altitude (ELA). We use a hybrid stress balance scheme in PISM (shallow ice approximation + shallow shelf approximation) and a thickness-based calving criterion. The horizontal resolution is 20 km. it includes three ELA decreasing speeds (ELA gradually decreases in 20 kyr, 100kyr, and step changes).
format Other/Unknown Material
author Weiwen Ji
author_facet Weiwen Ji
author_sort Weiwen Ji
title Laurentide ice saddle mergers drive rapid sea level drops during glaciations
title_short Laurentide ice saddle mergers drive rapid sea level drops during glaciations
title_full Laurentide ice saddle mergers drive rapid sea level drops during glaciations
title_fullStr Laurentide ice saddle mergers drive rapid sea level drops during glaciations
title_full_unstemmed Laurentide ice saddle mergers drive rapid sea level drops during glaciations
title_sort laurentide ice saddle mergers drive rapid sea level drops during glaciations
publisher Zenodo
publishDate 2021
url https://doi.org/10.5281/zenodo.4751076
genre Ice Sheet
genre_facet Ice Sheet
op_relation https://doi.org/10.5281/zenodo.4751075
https://doi.org/10.5281/zenodo.4751076
oai:zenodo.org:4751076
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.5281/zenodo.475107610.5281/zenodo.4751075
_version_ 1810449774861615104

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