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 contri...

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Published in:Earth System Dynamics
Main Authors: Gangadharan, Nidheesh, Goosse, Hugues, Parkes, David C., Goelzer, Heiko, Maussion, Fabien, Marzeion, Ben
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:https://hdl.handle.net/11250/3090733
https://doi.org/10.5194/esd-13-1417-2022
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spelling ftnorce:oai:norceresearch.brage.unit.no:11250/3090733 2023-10-25T01:31:23+02:00 Process-based estimate of global-mean sea-level changes in the Common Era Gangadharan, Nidheesh Goosse, Hugues Parkes, David C. Goelzer, Heiko Maussion, Fabien Marzeion, Ben 2022 application/pdf https://hdl.handle.net/11250/3090733 https://doi.org/10.5194/esd-13-1417-2022 eng eng Sigma2: NS9560K Sigma2: NS8006K Sigma2: NS5011K Norges forskningsråd: 295046 Sigma2: NN9560K Norges forskningsråd: 270061 Sigma2: NN8006K Norges forskningsråd: 324639 Earth System Dynamics (ESD). 2022, 13 (4), 1417-1435. urn:issn:2190-4979 https://hdl.handle.net/11250/3090733 https://doi.org/10.5194/esd-13-1417-2022 cristin:2068245 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no © Author(s) 2022 Earth System Dynamics (ESD) 13 4 1417-1435 Havnivå Sea level Klimadynamikk Climate dynamics VDP::Matematikk og naturvitenskap: 400 VDP::Mathematics and natural scienses: 400 Journal article Peer reviewed 2022 ftnorce https://doi.org/10.5194/esd-13-1417-2022 2023-09-27T22:49:50Z 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. publishedVersion Article in Journal/Newspaper Antarc* Antarctic glacier Greenland Ice Sheet NORCE vitenarkiv (Norwegian Research Centre) Antarctic Greenland The Antarctic Earth System Dynamics 13 4 1417 1435
institution Open Polar
collection NORCE vitenarkiv (Norwegian Research Centre)
op_collection_id ftnorce
language English
topic Havnivå
Sea level
Klimadynamikk
Climate dynamics
VDP::Matematikk og naturvitenskap: 400
VDP::Mathematics and natural scienses: 400
spellingShingle Havnivå
Sea level
Klimadynamikk
Climate dynamics
VDP::Matematikk og naturvitenskap: 400
VDP::Mathematics and natural scienses: 400
Gangadharan, Nidheesh
Goosse, Hugues
Parkes, David C.
Goelzer, Heiko
Maussion, Fabien
Marzeion, Ben
Process-based estimate of global-mean sea-level changes in the Common Era
topic_facet Havnivå
Sea level
Klimadynamikk
Climate dynamics
VDP::Matematikk og naturvitenskap: 400
VDP::Mathematics and natural scienses: 400
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. publishedVersion
format Article in Journal/Newspaper
author Gangadharan, Nidheesh
Goosse, Hugues
Parkes, David C.
Goelzer, Heiko
Maussion, Fabien
Marzeion, Ben
author_facet Gangadharan, Nidheesh
Goosse, Hugues
Parkes, David C.
Goelzer, Heiko
Maussion, Fabien
Marzeion, Ben
author_sort 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
publishDate 2022
url https://hdl.handle.net/11250/3090733
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 (ESD)
13
4
1417-1435
op_relation Sigma2: NS9560K
Sigma2: NS8006K
Sigma2: NS5011K
Norges forskningsråd: 295046
Sigma2: NN9560K
Norges forskningsråd: 270061
Sigma2: NN8006K
Norges forskningsråd: 324639
Earth System Dynamics (ESD). 2022, 13 (4), 1417-1435.
urn:issn:2190-4979
https://hdl.handle.net/11250/3090733
https://doi.org/10.5194/esd-13-1417-2022
cristin:2068245
op_rights Navngivelse 4.0 Internasjonal
http://creativecommons.org/licenses/by/4.0/deed.no
© Author(s) 2022
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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