Contribution of the Greenland Ice Sheet to sea-level over the next millennium using Large Ensemble Simulations, final state in year 3007 part 2, 2008-3007

The Greenland Ice Sheet holds around 7.2 meters of sea-level equivalent. In recent decades rising atmosphere and ocean temperatures have led to an acceleration in mass loss, adding an average of about 0.5 millimeters per year to global mean sea-level between 1991 and 2015. Current ice margin recessi...

Full description

Bibliographic Details
Main Author: Aschwanden, Andy
Format: Dataset
Language:English
Published: Arctic Data Center 2019
Subjects:
Online Access:https://dx.doi.org/10.18739/a2ns0kx61
https://arcticdata.io/catalog/#view/doi:10.18739/A2NS0KX61
id ftdatacite:10.18739/a2ns0kx61
record_format openpolar
spelling ftdatacite:10.18739/a2ns0kx61 2023-05-15T16:21:18+02:00 Contribution of the Greenland Ice Sheet to sea-level over the next millennium using Large Ensemble Simulations, final state in year 3007 part 2, 2008-3007 Aschwanden, Andy 2019 text/xml https://dx.doi.org/10.18739/a2ns0kx61 https://arcticdata.io/catalog/#view/doi:10.18739/A2NS0KX61 en eng Arctic Data Center ice sheets cryosphere models PISM ice sheet model dataset Dataset 2019 ftdatacite https://doi.org/10.18739/a2ns0kx61 2021-11-05T12:55:41Z The Greenland Ice Sheet holds around 7.2 meters of sea-level equivalent. In recent decades rising atmosphere and ocean temperatures have led to an acceleration in mass loss, adding an average of about 0.5 millimeters per year to global mean sea-level between 1991 and 2015. Current ice margin recession in Greenland is led by the retreat of outlet glaciers, the large rivers of ice ending in narrow fjords that drain the ice sheet interior. Recent progress in measuring ice thickness is enabling models to reproduce the complex flow patterns found in outlet glaciers, a key step towards realistic projections. Here we pair an outlet glacier resolving ice sheet model with a comprehensive uncertainty quantification to estimate Greenland's contribution to sea-level over the next millennium under different climate forcings. We find that Greenland could contribute 5-33 centimeters to sea-level by 2100 and 11-155 centimeters by 2200, with discharge from outlet glaciers contributing 6-45% of the total mass loss. Our analysis shows that uncertainties in projecting mass loss are dominated by uncertainties in climate scenarios and surface processes, followed by ice dynamics, whereas uncertainties in ocean conditions play a minor role, particularly in the long term. We project that Greenland will very likely become ice-free within a millennium without significant reductions in greenhouse gas emissions. This dataset compilation contains the simulations for the manuscript "Contribution of the Greenland Ice Sheet to sea-level over the next millennium" prepared with the Parallel Ice Sheet Model (PISM). This dataset provides the final states at the year 3007 of the simulations that succesfully finished (some simulations did not converge) for the RCPs (Representative Concentration Pathways) 2.6, 4.5, and 8.5 for LES (Large Ensemble Simulation) ids 000-499. Dataset glacier Greenland Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Greenland
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic ice sheets
cryosphere models
PISM
ice sheet model
spellingShingle ice sheets
cryosphere models
PISM
ice sheet model
Aschwanden, Andy
Contribution of the Greenland Ice Sheet to sea-level over the next millennium using Large Ensemble Simulations, final state in year 3007 part 2, 2008-3007
topic_facet ice sheets
cryosphere models
PISM
ice sheet model
description The Greenland Ice Sheet holds around 7.2 meters of sea-level equivalent. In recent decades rising atmosphere and ocean temperatures have led to an acceleration in mass loss, adding an average of about 0.5 millimeters per year to global mean sea-level between 1991 and 2015. Current ice margin recession in Greenland is led by the retreat of outlet glaciers, the large rivers of ice ending in narrow fjords that drain the ice sheet interior. Recent progress in measuring ice thickness is enabling models to reproduce the complex flow patterns found in outlet glaciers, a key step towards realistic projections. Here we pair an outlet glacier resolving ice sheet model with a comprehensive uncertainty quantification to estimate Greenland's contribution to sea-level over the next millennium under different climate forcings. We find that Greenland could contribute 5-33 centimeters to sea-level by 2100 and 11-155 centimeters by 2200, with discharge from outlet glaciers contributing 6-45% of the total mass loss. Our analysis shows that uncertainties in projecting mass loss are dominated by uncertainties in climate scenarios and surface processes, followed by ice dynamics, whereas uncertainties in ocean conditions play a minor role, particularly in the long term. We project that Greenland will very likely become ice-free within a millennium without significant reductions in greenhouse gas emissions. This dataset compilation contains the simulations for the manuscript "Contribution of the Greenland Ice Sheet to sea-level over the next millennium" prepared with the Parallel Ice Sheet Model (PISM). This dataset provides the final states at the year 3007 of the simulations that succesfully finished (some simulations did not converge) for the RCPs (Representative Concentration Pathways) 2.6, 4.5, and 8.5 for LES (Large Ensemble Simulation) ids 000-499.
format Dataset
author Aschwanden, Andy
author_facet Aschwanden, Andy
author_sort Aschwanden, Andy
title Contribution of the Greenland Ice Sheet to sea-level over the next millennium using Large Ensemble Simulations, final state in year 3007 part 2, 2008-3007
title_short Contribution of the Greenland Ice Sheet to sea-level over the next millennium using Large Ensemble Simulations, final state in year 3007 part 2, 2008-3007
title_full Contribution of the Greenland Ice Sheet to sea-level over the next millennium using Large Ensemble Simulations, final state in year 3007 part 2, 2008-3007
title_fullStr Contribution of the Greenland Ice Sheet to sea-level over the next millennium using Large Ensemble Simulations, final state in year 3007 part 2, 2008-3007
title_full_unstemmed Contribution of the Greenland Ice Sheet to sea-level over the next millennium using Large Ensemble Simulations, final state in year 3007 part 2, 2008-3007
title_sort contribution of the greenland ice sheet to sea-level over the next millennium using large ensemble simulations, final state in year 3007 part 2, 2008-3007
publisher Arctic Data Center
publishDate 2019
url https://dx.doi.org/10.18739/a2ns0kx61
https://arcticdata.io/catalog/#view/doi:10.18739/A2NS0KX61
geographic Greenland
geographic_facet Greenland
genre glacier
Greenland
Ice Sheet
genre_facet glacier
Greenland
Ice Sheet
op_doi https://doi.org/10.18739/a2ns0kx61
_version_ 1766009314330279936