Process-based estimate of global-mean sea-level changes in the Common Era
Although the global-mean sea level (GMSL) rose over the twentieth century with a positive contribution from thermosteric and barystatic (ice sheets and glaciers) sources, the driving processes of GMSL changes during the pre-industrial Common Era (PCE; 1–1850 CE) are largely unknown. Here, the cont...
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Online Access: | http://hdl.handle.net/2078.1/265894 https://doi.org/10.5194/esd-13-1417-2022 |
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ftunistlouisbrus:oai:dial.uclouvain.be:boreal:265894 2024-05-12T07:55:28+00:00 Process-based estimate of global-mean sea-level changes in the Common Era Ayiraveetil Gangadharan, Nidheesh Goosse, Hugues Parkes, David Goelzer, Heiko Maussion, Fabien Marzeion, Ben UCL - SST/ELI/ELIC - Earth & Climate 2022 http://hdl.handle.net/2078.1/265894 https://doi.org/10.5194/esd-13-1417-2022 eng eng Copernicus GmbH boreal:265894 http://hdl.handle.net/2078.1/265894 doi:10.5194/esd-13-1417-2022 urn:ISSN:2190-4979 urn:EISSN:2190-4987 info:eu-repo/semantics/openAccess Earth System Dynamics, Vol. 13, no.4, p. 1417-1435 (2022) General Earth and Planetary Sciences info:eu-repo/semantics/article 2022 ftunistlouisbrus https://doi.org/10.5194/esd-13-1417-2022 2024-04-18T17:11:06Z Although the global-mean sea level (GMSL) rose over the twentieth century with a positive contribution from thermosteric and barystatic (ice sheets and glaciers) sources, the driving processes of GMSL changes during the pre-industrial Common Era (PCE; 1–1850 CE) are largely unknown. Here, the contributions of glacier and ice sheet mass variations and ocean thermal expansion to GMSL in the Common Era (1–2000 CE) are estimated based on simulations with different physical models. Although the twentieth century global-mean thermosteric sea level (GMTSL) is mainly associated with temperature variations in the upper 700 m (86 % in reconstruction and 74 ± 8 % in model), GMTSL in the PCE is equally controlled by temperature changes below 700 m. The GMTSL does not vary more than ±2 cm during the PCE. GMSL contributions from the Antarctic and Greenland ice sheets tend to cancel each other out during the PCE owing to the differing response of the two ice sheets to atmospheric conditions. The uncertainties of sea-level contribution from land-ice mass variations are large, especially over the first millennium. Despite underestimating the twentieth century model GMSL, there is a general agreement between the model and proxy-based GMSL reconstructions in the CE. Although the uncertainties remain large over the first millennium, model simulations point to glaciers as the dominant source of GMSL changes during the PCE. Article in Journal/Newspaper Antarc* Antarctic glacier Greenland Ice Sheet DIAL@USL-B (Université Saint-Louis, Bruxelles) Antarctic Greenland The Antarctic Earth System Dynamics 13 4 1417 1435 |
institution |
Open Polar |
collection |
DIAL@USL-B (Université Saint-Louis, Bruxelles) |
op_collection_id |
ftunistlouisbrus |
language |
English |
topic |
General Earth and Planetary Sciences |
spellingShingle |
General Earth and Planetary Sciences Ayiraveetil Gangadharan, Nidheesh Goosse, Hugues Parkes, David Goelzer, Heiko Maussion, Fabien Marzeion, Ben Process-based estimate of global-mean sea-level changes in the Common Era |
topic_facet |
General Earth and Planetary Sciences |
description |
Although the global-mean sea level (GMSL) rose over the twentieth century with a positive contribution from thermosteric and barystatic (ice sheets and glaciers) sources, the driving processes of GMSL changes during the pre-industrial Common Era (PCE; 1–1850 CE) are largely unknown. Here, the contributions of glacier and ice sheet mass variations and ocean thermal expansion to GMSL in the Common Era (1–2000 CE) are estimated based on simulations with different physical models. Although the twentieth century global-mean thermosteric sea level (GMTSL) is mainly associated with temperature variations in the upper 700 m (86 % in reconstruction and 74 ± 8 % in model), GMTSL in the PCE is equally controlled by temperature changes below 700 m. The GMTSL does not vary more than ±2 cm during the PCE. GMSL contributions from the Antarctic and Greenland ice sheets tend to cancel each other out during the PCE owing to the differing response of the two ice sheets to atmospheric conditions. The uncertainties of sea-level contribution from land-ice mass variations are large, especially over the first millennium. Despite underestimating the twentieth century model GMSL, there is a general agreement between the model and proxy-based GMSL reconstructions in the CE. Although the uncertainties remain large over the first millennium, model simulations point to glaciers as the dominant source of GMSL changes during the PCE. |
author2 |
UCL - SST/ELI/ELIC - Earth & Climate |
format |
Article in Journal/Newspaper |
author |
Ayiraveetil Gangadharan, Nidheesh Goosse, Hugues Parkes, David Goelzer, Heiko Maussion, Fabien Marzeion, Ben |
author_facet |
Ayiraveetil Gangadharan, Nidheesh Goosse, Hugues Parkes, David Goelzer, Heiko Maussion, Fabien Marzeion, Ben |
author_sort |
Ayiraveetil Gangadharan, Nidheesh |
title |
Process-based estimate of global-mean sea-level changes in the Common Era |
title_short |
Process-based estimate of global-mean sea-level changes in the Common Era |
title_full |
Process-based estimate of global-mean sea-level changes in the Common Era |
title_fullStr |
Process-based estimate of global-mean sea-level changes in the Common Era |
title_full_unstemmed |
Process-based estimate of global-mean sea-level changes in the Common Era |
title_sort |
process-based estimate of global-mean sea-level changes in the common era |
publisher |
Copernicus GmbH |
publishDate |
2022 |
url |
http://hdl.handle.net/2078.1/265894 https://doi.org/10.5194/esd-13-1417-2022 |
geographic |
Antarctic Greenland The Antarctic |
geographic_facet |
Antarctic Greenland The Antarctic |
genre |
Antarc* Antarctic glacier Greenland Ice Sheet |
genre_facet |
Antarc* Antarctic glacier Greenland Ice Sheet |
op_source |
Earth System Dynamics, Vol. 13, no.4, p. 1417-1435 (2022) |
op_relation |
boreal:265894 http://hdl.handle.net/2078.1/265894 doi:10.5194/esd-13-1417-2022 urn:ISSN:2190-4979 urn:EISSN:2190-4987 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/esd-13-1417-2022 |
container_title |
Earth System Dynamics |
container_volume |
13 |
container_issue |
4 |
container_start_page |
1417 |
op_container_end_page |
1435 |
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1798835254760308736 |