Simulations of Miocene Antarctic ice-sheet variability under increased precipitation and sub-shelf melt, using the ice-sheet model IMAU-ICE ...

To demonstrate the viability of a precipitation regime change leading to a fundamentally different volume-to-area ratio of the Antarctic ice sheet, we deploy the 3D thermodynamical ice sheet/shelf model IMAU-ICE v1.1.1. In the standard set-up (Stap et al., 2021a, 2021b), climate forcing follows from...

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Main Authors: Stap, Lennert B., Hou, Suning, Bijl, Peter K.
Format: Dataset
Language:English
Published: Zenodo 2023
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.8308285
https://zenodo.org/doi/10.5281/zenodo.8308285
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author Stap, Lennert B.
Hou, Suning
Bijl, Peter K.
author_facet Stap, Lennert B.
Hou, Suning
Bijl, Peter K.
author_sort Stap, Lennert B.
collection DataCite
description To demonstrate the viability of a precipitation regime change leading to a fundamentally different volume-to-area ratio of the Antarctic ice sheet, we deploy the 3D thermodynamical ice sheet/shelf model IMAU-ICE v1.1.1. In the standard set-up (Stap et al., 2021a, 2021b), climate forcing follows from pre-run warm and cold snapshot climate simulations. The applied climate forcing is transiently calculated based on the prescribed CO2 concentration and the modelled ice sheet size, through a matrix interpolation method. Equilibrium experiments are performed at various CO2 levels between preindustrial and 3x preindustrial CO2 values, with insolation at present-day levels and initiated from an ice-free Miocene Antarctic topography (dataset Hochmuth et al., 2020). Here, we perform additional sensitivity experiments, in which we apply a fixed precipitation increase and extreme sub-shelf melt rates. The precipitation anomaly is calculated as 25% of the warm snapshot precipitation fields, sub-shelf melt rates are set ... : L.B. Stap is funded by the Dutch Research Council (NWO), through VENI grant VI.Veni.202.031. Simulations were performed on the Gemini computing cluster of the Faculty of Science, Utrecht University. ...
format Dataset
genre Antarc*
Antarctic
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
geographic Antarctic
Gemini
The Antarctic
geographic_facet Antarctic
Gemini
The Antarctic
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long_lat ENVELOPE(-62.500,-62.500,-66.133,-66.133)
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op_doi https://doi.org/10.5281/zenodo.830828510.5281/zenodo.8308286
op_relation https://dx.doi.org/10.5281/zenodo.8308286
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
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spelling ftdatacite:10.5281/zenodo.8308285 2025-01-16T19:37:31+00:00 Simulations of Miocene Antarctic ice-sheet variability under increased precipitation and sub-shelf melt, using the ice-sheet model IMAU-ICE ... Stap, Lennert B. Hou, Suning Bijl, Peter K. 2023 https://dx.doi.org/10.5281/zenodo.8308285 https://zenodo.org/doi/10.5281/zenodo.8308285 en eng Zenodo https://dx.doi.org/10.5281/zenodo.8308286 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Antarctic ice sheet Antarctica Miocene Paleoclimate Mid-Miocene Climate Transition Dataset dataset 2023 ftdatacite https://doi.org/10.5281/zenodo.830828510.5281/zenodo.8308286 2023-11-03T10:55:20Z To demonstrate the viability of a precipitation regime change leading to a fundamentally different volume-to-area ratio of the Antarctic ice sheet, we deploy the 3D thermodynamical ice sheet/shelf model IMAU-ICE v1.1.1. In the standard set-up (Stap et al., 2021a, 2021b), climate forcing follows from pre-run warm and cold snapshot climate simulations. The applied climate forcing is transiently calculated based on the prescribed CO2 concentration and the modelled ice sheet size, through a matrix interpolation method. Equilibrium experiments are performed at various CO2 levels between preindustrial and 3x preindustrial CO2 values, with insolation at present-day levels and initiated from an ice-free Miocene Antarctic topography (dataset Hochmuth et al., 2020). Here, we perform additional sensitivity experiments, in which we apply a fixed precipitation increase and extreme sub-shelf melt rates. The precipitation anomaly is calculated as 25% of the warm snapshot precipitation fields, sub-shelf melt rates are set ... : L.B. Stap is funded by the Dutch Research Council (NWO), through VENI grant VI.Veni.202.031. Simulations were performed on the Gemini computing cluster of the Faculty of Science, Utrecht University. ... Dataset Antarc* Antarctic Antarctica Ice Sheet DataCite Antarctic Gemini ENVELOPE(-62.500,-62.500,-66.133,-66.133) The Antarctic
spellingShingle Antarctic ice sheet
Antarctica
Miocene
Paleoclimate
Mid-Miocene Climate Transition
Stap, Lennert B.
Hou, Suning
Bijl, Peter K.
Simulations of Miocene Antarctic ice-sheet variability under increased precipitation and sub-shelf melt, using the ice-sheet model IMAU-ICE ...
title Simulations of Miocene Antarctic ice-sheet variability under increased precipitation and sub-shelf melt, using the ice-sheet model IMAU-ICE ...
title_full Simulations of Miocene Antarctic ice-sheet variability under increased precipitation and sub-shelf melt, using the ice-sheet model IMAU-ICE ...
title_fullStr Simulations of Miocene Antarctic ice-sheet variability under increased precipitation and sub-shelf melt, using the ice-sheet model IMAU-ICE ...
title_full_unstemmed Simulations of Miocene Antarctic ice-sheet variability under increased precipitation and sub-shelf melt, using the ice-sheet model IMAU-ICE ...
title_short Simulations of Miocene Antarctic ice-sheet variability under increased precipitation and sub-shelf melt, using the ice-sheet model IMAU-ICE ...
title_sort simulations of miocene antarctic ice-sheet variability under increased precipitation and sub-shelf melt, using the ice-sheet model imau-ice ...
topic Antarctic ice sheet
Antarctica
Miocene
Paleoclimate
Mid-Miocene Climate Transition
topic_facet Antarctic ice sheet
Antarctica
Miocene
Paleoclimate
Mid-Miocene Climate Transition
url https://dx.doi.org/10.5281/zenodo.8308285
https://zenodo.org/doi/10.5281/zenodo.8308285