The future sea-level contribution of the Greenland ice sheet: A multi-model ensemble study of ISMIP6
The Greenland ice sheet is one of the largest contributors to global mean sea-level rise today and is expected to continue to lose mass as the Arctic continues to warm. The two predominant mass loss mechanisms are increased surface meltwater run-off and mass loss associated with the retreat of marin...
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2020
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Online Access: | https://oa.tib.eu/renate/handle/123456789/10566 https://doi.org/10.34657/9602 |
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ftleibnizopen:oai:oai.leibnizopen.de:ci_ReYsBBwLIz6xGzNmY 2023-11-12T04:12:27+01:00 The future sea-level contribution of the Greenland ice sheet: A multi-model ensemble study of ISMIP6 Goelzer, Heiko Nowicki, Sophie Payne, Anthony Larour, Eric Seroussi, Helene Lipscomb, William H. Gregory, Jonathan Abe-Ouchi, Ayako Shepherd, Andrew Simon, Erika Agosta, Cécile Alexander, Patrick Aschwanden, Andy Barthel, Alice Calov, Reinhard Chambers, Christopher Choi, Youngmin Cuzzone, Joshua Dumas, Christophe Edwards, Tamsin Felikson, Denis Fettweis, Xavier Golledge, Nicholas R. Greve, Ralf Humbert, Angelika Huybrechts, Philippe Le clec'h, Sebastien Lee, Victoria Leguy, Gunter Little, Chris Lowry, Daniel P. Morlighem, Mathieu Nias, Isabel Quiquet, Aurelien Rückamp, Martin Schlegel, Nicole-Jeanne Slater, Donald A. Smith, Robin S. Straneo, Fiammetta Tarasov, Lev van de Wal, Roderik van den Broeke, Michiel 2020 application/pdf https://oa.tib.eu/renate/handle/123456789/10566 https://doi.org/10.34657/9602 eng eng Katlenburg-Lindau : Copernicus CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/ The Cryosphere 14 (2020), Nr. 9 climate modeling CMIP ensemble forecasting global climate greenhouse gas ice retreat meltwater model runoff sea level change Arctic Arctic Ocean Greenland Greenland Ice Sheet 550 article Text 2020 ftleibnizopen https://doi.org/10.34657/9602 2023-10-30T00:35:28Z The Greenland ice sheet is one of the largest contributors to global mean sea-level rise today and is expected to continue to lose mass as the Arctic continues to warm. The two predominant mass loss mechanisms are increased surface meltwater run-off and mass loss associated with the retreat of marine-terminating outlet glaciers. In this paper we use a large ensemble of Greenland ice sheet models forced by output from a representative subset of the Coupled Model Intercomparison Project (CMIP5) global climate models to project ice sheet changes and sea-level rise contributions over the 21st century. The simulations are part of the Ice Sheet Model Intercomparison Project for CMIP6 (ISMIP6).We estimate the sea-level contribution together with uncertainties due to future climate forcing, ice sheet model formulations and ocean forcing for the two greenhouse gas concentration scenarios RCP8.5 and RCP2.6. The results indicate that the Greenland ice sheet will continue to lose mass in both scenarios until 2100, with contributions of 90-50 and 32-17mm to sea-level rise for RCP8.5 and RCP2.6, respectively. The largest mass loss is expected from the south-west of Greenland, which is governed by surface mass balance changes, continuing what is already observed today. Because the contributions are calculated against an unforced control experiment, these numbers do not include any committed mass loss, i.e. mass loss that would occur over the coming century if the climate forcing remained constant. Under RCP8.5 forcing, ice sheet model uncertainty explains an ensemble spread of 40 mm, while climate model uncertainty and ocean forcing uncertainty account for a spread of 36 and 19 mm, respectively. Apart from those formally derived uncertainty ranges, the largest gap in our knowledge is about the physical understanding and implementation of the calving process, i.e. the interaction of the ice sheet with the ocean. © Author(s) 2020. publishedVersion Article in Journal/Newspaper Arctic Arctic Ocean Greenland Ice Sheet The Cryosphere Unknown |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftleibnizopen |
language |
English |
topic |
climate modeling CMIP ensemble forecasting global climate greenhouse gas ice retreat meltwater model runoff sea level change Arctic Arctic Ocean Greenland Greenland Ice Sheet 550 |
spellingShingle |
climate modeling CMIP ensemble forecasting global climate greenhouse gas ice retreat meltwater model runoff sea level change Arctic Arctic Ocean Greenland Greenland Ice Sheet 550 Goelzer, Heiko Nowicki, Sophie Payne, Anthony Larour, Eric Seroussi, Helene Lipscomb, William H. Gregory, Jonathan Abe-Ouchi, Ayako Shepherd, Andrew Simon, Erika Agosta, Cécile Alexander, Patrick Aschwanden, Andy Barthel, Alice Calov, Reinhard Chambers, Christopher Choi, Youngmin Cuzzone, Joshua Dumas, Christophe Edwards, Tamsin Felikson, Denis Fettweis, Xavier Golledge, Nicholas R. Greve, Ralf Humbert, Angelika Huybrechts, Philippe Le clec'h, Sebastien Lee, Victoria Leguy, Gunter Little, Chris Lowry, Daniel P. Morlighem, Mathieu Nias, Isabel Quiquet, Aurelien Rückamp, Martin Schlegel, Nicole-Jeanne Slater, Donald A. Smith, Robin S. Straneo, Fiammetta Tarasov, Lev van de Wal, Roderik van den Broeke, Michiel The future sea-level contribution of the Greenland ice sheet: A multi-model ensemble study of ISMIP6 |
topic_facet |
climate modeling CMIP ensemble forecasting global climate greenhouse gas ice retreat meltwater model runoff sea level change Arctic Arctic Ocean Greenland Greenland Ice Sheet 550 |
description |
The Greenland ice sheet is one of the largest contributors to global mean sea-level rise today and is expected to continue to lose mass as the Arctic continues to warm. The two predominant mass loss mechanisms are increased surface meltwater run-off and mass loss associated with the retreat of marine-terminating outlet glaciers. In this paper we use a large ensemble of Greenland ice sheet models forced by output from a representative subset of the Coupled Model Intercomparison Project (CMIP5) global climate models to project ice sheet changes and sea-level rise contributions over the 21st century. The simulations are part of the Ice Sheet Model Intercomparison Project for CMIP6 (ISMIP6).We estimate the sea-level contribution together with uncertainties due to future climate forcing, ice sheet model formulations and ocean forcing for the two greenhouse gas concentration scenarios RCP8.5 and RCP2.6. The results indicate that the Greenland ice sheet will continue to lose mass in both scenarios until 2100, with contributions of 90-50 and 32-17mm to sea-level rise for RCP8.5 and RCP2.6, respectively. The largest mass loss is expected from the south-west of Greenland, which is governed by surface mass balance changes, continuing what is already observed today. Because the contributions are calculated against an unforced control experiment, these numbers do not include any committed mass loss, i.e. mass loss that would occur over the coming century if the climate forcing remained constant. Under RCP8.5 forcing, ice sheet model uncertainty explains an ensemble spread of 40 mm, while climate model uncertainty and ocean forcing uncertainty account for a spread of 36 and 19 mm, respectively. Apart from those formally derived uncertainty ranges, the largest gap in our knowledge is about the physical understanding and implementation of the calving process, i.e. the interaction of the ice sheet with the ocean. © Author(s) 2020. publishedVersion |
format |
Article in Journal/Newspaper |
author |
Goelzer, Heiko Nowicki, Sophie Payne, Anthony Larour, Eric Seroussi, Helene Lipscomb, William H. Gregory, Jonathan Abe-Ouchi, Ayako Shepherd, Andrew Simon, Erika Agosta, Cécile Alexander, Patrick Aschwanden, Andy Barthel, Alice Calov, Reinhard Chambers, Christopher Choi, Youngmin Cuzzone, Joshua Dumas, Christophe Edwards, Tamsin Felikson, Denis Fettweis, Xavier Golledge, Nicholas R. Greve, Ralf Humbert, Angelika Huybrechts, Philippe Le clec'h, Sebastien Lee, Victoria Leguy, Gunter Little, Chris Lowry, Daniel P. Morlighem, Mathieu Nias, Isabel Quiquet, Aurelien Rückamp, Martin Schlegel, Nicole-Jeanne Slater, Donald A. Smith, Robin S. Straneo, Fiammetta Tarasov, Lev van de Wal, Roderik van den Broeke, Michiel |
author_facet |
Goelzer, Heiko Nowicki, Sophie Payne, Anthony Larour, Eric Seroussi, Helene Lipscomb, William H. Gregory, Jonathan Abe-Ouchi, Ayako Shepherd, Andrew Simon, Erika Agosta, Cécile Alexander, Patrick Aschwanden, Andy Barthel, Alice Calov, Reinhard Chambers, Christopher Choi, Youngmin Cuzzone, Joshua Dumas, Christophe Edwards, Tamsin Felikson, Denis Fettweis, Xavier Golledge, Nicholas R. Greve, Ralf Humbert, Angelika Huybrechts, Philippe Le clec'h, Sebastien Lee, Victoria Leguy, Gunter Little, Chris Lowry, Daniel P. Morlighem, Mathieu Nias, Isabel Quiquet, Aurelien Rückamp, Martin Schlegel, Nicole-Jeanne Slater, Donald A. Smith, Robin S. Straneo, Fiammetta Tarasov, Lev van de Wal, Roderik van den Broeke, Michiel |
author_sort |
Goelzer, Heiko |
title |
The future sea-level contribution of the Greenland ice sheet: A multi-model ensemble study of ISMIP6 |
title_short |
The future sea-level contribution of the Greenland ice sheet: A multi-model ensemble study of ISMIP6 |
title_full |
The future sea-level contribution of the Greenland ice sheet: A multi-model ensemble study of ISMIP6 |
title_fullStr |
The future sea-level contribution of the Greenland ice sheet: A multi-model ensemble study of ISMIP6 |
title_full_unstemmed |
The future sea-level contribution of the Greenland ice sheet: A multi-model ensemble study of ISMIP6 |
title_sort |
future sea-level contribution of the greenland ice sheet: a multi-model ensemble study of ismip6 |
publisher |
Katlenburg-Lindau : Copernicus |
publishDate |
2020 |
url |
https://oa.tib.eu/renate/handle/123456789/10566 https://doi.org/10.34657/9602 |
genre |
Arctic Arctic Ocean Greenland Ice Sheet The Cryosphere |
genre_facet |
Arctic Arctic Ocean Greenland Ice Sheet The Cryosphere |
op_source |
The Cryosphere 14 (2020), Nr. 9 |
op_rights |
CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.34657/9602 |
_version_ |
1782330977863860224 |