Data from: Subglacial discharge accelerates future retreat of Denman and Scott Glaciers, East Antarctica ...

Ice shelf basal melting is the primary mechanism driving mass loss from the Antarctic Ice Sheet, yet it is unknown how the localized melt enhancement from subglacial discharge will impact future Antarctic glacial retreat. Here, we develop a parameterization of ice shelf basal melt that accounts for...

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Main Authors: Pelle, Tyler, Greenbaum, Jamin, Dow, Christine, Jenkins, Adrian, Morlighem, Mathieu
Format: Dataset
Language:English
Published: Dryad 2022
Subjects:
Online Access:https://dx.doi.org/10.7280/d1x12s
https://datadryad.org/stash/dataset/doi:10.7280/D1X12S
id ftdatacite:10.7280/d1x12s
record_format openpolar
spelling ftdatacite:10.7280/d1x12s 2024-04-28T07:57:11+00:00 Data from: Subglacial discharge accelerates future retreat of Denman and Scott Glaciers, East Antarctica ... Pelle, Tyler Greenbaum, Jamin Dow, Christine Jenkins, Adrian Morlighem, Mathieu 2022 https://dx.doi.org/10.7280/d1x12s https://datadryad.org/stash/dataset/doi:10.7280/D1X12S en eng Dryad Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode cc0-1.0 Antarctica FOS Earth and related environmental sciences ice sheet modeling Climate change Sea level rise subglacial discharge Glaciology glacier retreat dataset Dataset 2022 ftdatacite https://doi.org/10.7280/d1x12s 2024-04-02T11:56:20Z Ice shelf basal melting is the primary mechanism driving mass loss from the Antarctic Ice Sheet, yet it is unknown how the localized melt enhancement from subglacial discharge will impact future Antarctic glacial retreat. Here, we develop a parameterization of ice shelf basal melt that accounts for both ocean and subglacial discharge forcing and apply it in future projections of Denman and Scott Glaciers, East Antarctica, through 2300. In forward simulations, subglacial discharge accelerates retreat of these systems into the deepest continental trench on Earth by 25 years. During this retreat, Denman Glacier alone contributes 0.33 mm/yr to global sea level rise, comparable to half of the contemporary sea level contribution of the entire Antarctic Ice Sheet. Our results stress the importance of resolving complex interactions between the ice, ocean, and subglacial environments in future Antarctic Ice Sheet projections. In this data publication, we present the model output and results associated with the ... : Ice sheet model results: Direct results taken from the Ice-sheet and Sea-level System Model (ISSM, Larour et al. 2012) with no processing applied, provided yearly as *.mat files. Ice sheet model initial state: Initial state (ice geometry, mesh information, inversion results, etc.) of the ice sheet model containing Denman and Scott Galciers with no processing applied, provided as a *.mat file. The contents of the *.mat file is a MATLAB variable of class "model", which is compatible with ISSM. Melt parameterization script: Documented MATLAB script ready to run with the provided data sets. Ocean temperature and salinity timeseries: Bottom ocean temperature (°C) and salinity (PSU) timeseries (January 1st, 2017 through December 31, 2299) extracted from an East Antarctic configuration of the ocean component of the MITgcm (Pelle et al., 2021). Temperature and salinity were averaged bi-weekly along the ice fronts of Denman and Scott Glaciers (see white dashed contour in figure 1a of the main manuscript text) along ... Dataset Antarc* Antarctic Antarctica Denman Glacier East Antarctica Ice Sheet Ice Shelf DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Antarctica
FOS Earth and related environmental sciences
ice sheet modeling
Climate change
Sea level rise
subglacial discharge
Glaciology
glacier retreat
spellingShingle Antarctica
FOS Earth and related environmental sciences
ice sheet modeling
Climate change
Sea level rise
subglacial discharge
Glaciology
glacier retreat
Pelle, Tyler
Greenbaum, Jamin
Dow, Christine
Jenkins, Adrian
Morlighem, Mathieu
Data from: Subglacial discharge accelerates future retreat of Denman and Scott Glaciers, East Antarctica ...
topic_facet Antarctica
FOS Earth and related environmental sciences
ice sheet modeling
Climate change
Sea level rise
subglacial discharge
Glaciology
glacier retreat
description Ice shelf basal melting is the primary mechanism driving mass loss from the Antarctic Ice Sheet, yet it is unknown how the localized melt enhancement from subglacial discharge will impact future Antarctic glacial retreat. Here, we develop a parameterization of ice shelf basal melt that accounts for both ocean and subglacial discharge forcing and apply it in future projections of Denman and Scott Glaciers, East Antarctica, through 2300. In forward simulations, subglacial discharge accelerates retreat of these systems into the deepest continental trench on Earth by 25 years. During this retreat, Denman Glacier alone contributes 0.33 mm/yr to global sea level rise, comparable to half of the contemporary sea level contribution of the entire Antarctic Ice Sheet. Our results stress the importance of resolving complex interactions between the ice, ocean, and subglacial environments in future Antarctic Ice Sheet projections. In this data publication, we present the model output and results associated with the ... : Ice sheet model results: Direct results taken from the Ice-sheet and Sea-level System Model (ISSM, Larour et al. 2012) with no processing applied, provided yearly as *.mat files. Ice sheet model initial state: Initial state (ice geometry, mesh information, inversion results, etc.) of the ice sheet model containing Denman and Scott Galciers with no processing applied, provided as a *.mat file. The contents of the *.mat file is a MATLAB variable of class "model", which is compatible with ISSM. Melt parameterization script: Documented MATLAB script ready to run with the provided data sets. Ocean temperature and salinity timeseries: Bottom ocean temperature (°C) and salinity (PSU) timeseries (January 1st, 2017 through December 31, 2299) extracted from an East Antarctic configuration of the ocean component of the MITgcm (Pelle et al., 2021). Temperature and salinity were averaged bi-weekly along the ice fronts of Denman and Scott Glaciers (see white dashed contour in figure 1a of the main manuscript text) along ...
format Dataset
author Pelle, Tyler
Greenbaum, Jamin
Dow, Christine
Jenkins, Adrian
Morlighem, Mathieu
author_facet Pelle, Tyler
Greenbaum, Jamin
Dow, Christine
Jenkins, Adrian
Morlighem, Mathieu
author_sort Pelle, Tyler
title Data from: Subglacial discharge accelerates future retreat of Denman and Scott Glaciers, East Antarctica ...
title_short Data from: Subglacial discharge accelerates future retreat of Denman and Scott Glaciers, East Antarctica ...
title_full Data from: Subglacial discharge accelerates future retreat of Denman and Scott Glaciers, East Antarctica ...
title_fullStr Data from: Subglacial discharge accelerates future retreat of Denman and Scott Glaciers, East Antarctica ...
title_full_unstemmed Data from: Subglacial discharge accelerates future retreat of Denman and Scott Glaciers, East Antarctica ...
title_sort data from: subglacial discharge accelerates future retreat of denman and scott glaciers, east antarctica ...
publisher Dryad
publishDate 2022
url https://dx.doi.org/10.7280/d1x12s
https://datadryad.org/stash/dataset/doi:10.7280/D1X12S
genre Antarc*
Antarctic
Antarctica
Denman Glacier
East Antarctica
Ice Sheet
Ice Shelf
genre_facet Antarc*
Antarctic
Antarctica
Denman Glacier
East Antarctica
Ice Sheet
Ice Shelf
op_rights Creative Commons Zero v1.0 Universal
https://creativecommons.org/publicdomain/zero/1.0/legalcode
cc0-1.0
op_doi https://doi.org/10.7280/d1x12s
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