Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts?
Confidence in projections of global-mean sea level rise (GMSLR) depends on an ability to account for GMSLR during the twentieth century. There are contributions from ocean thermal expansion, mass loss from glaciers and ice sheets, groundwater extraction, and reservoir impoundment. Progress has been...
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Language: | English |
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American Meteorological Society
2013
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Online Access: | https://nrl.northumbria.ac.uk/id/eprint/13070/ https://doi.org/10.1175/JCLI-D-12-00319.1 https://nrl.northumbria.ac.uk/id/eprint/13070/1/leanne_wake_sealevelrise.pdf |
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ftunivnorthumb:oai:nrl.northumbria.ac.uk:13070 2023-05-15T13:35:33+02:00 Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts? Gregory, Jonathan White, Neil Church, John Bierkens, Marc Box, Jason van den Broeke, Michiel Cogley, Graham Fettweis, Xavier Hanna, Edward Huybrechts, Philippe Konikow, Leonard Leclercq, Paul Marzeion, Ben Oerlemans, Johannes Tamisiea, Mark Wada, Yoshihide Wake, Leanne van de Wal, Roderik 2013-07 application/pdf https://nrl.northumbria.ac.uk/id/eprint/13070/ https://doi.org/10.1175/JCLI-D-12-00319.1 https://nrl.northumbria.ac.uk/id/eprint/13070/1/leanne_wake_sealevelrise.pdf en eng American Meteorological Society https://nrl.northumbria.ac.uk/id/eprint/13070/1/leanne_wake_sealevelrise.pdf Gregory, Jonathan, White, Neil, Church, John, Bierkens, Marc, Box, Jason, van den Broeke, Michiel, Cogley, Graham, Fettweis, Xavier, Hanna, Edward, Huybrechts, Philippe, Konikow, Leonard, Leclercq, Paul, Marzeion, Ben, Oerlemans, Johannes, Tamisiea, Mark, Wada, Yoshihide, Wake, Leanne and van de Wal, Roderik (2013) Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts? Journal of Climate, 26 (13). pp. 4476-4499. ISSN 0894-8755 F800 Physical and Terrestrial Geographical and Environmental Sciences Article PeerReviewed 2013 ftunivnorthumb https://doi.org/10.1175/JCLI-D-12-00319.1 2022-09-25T05:57:53Z Confidence in projections of global-mean sea level rise (GMSLR) depends on an ability to account for GMSLR during the twentieth century. There are contributions from ocean thermal expansion, mass loss from glaciers and ice sheets, groundwater extraction, and reservoir impoundment. Progress has been made toward solving the “enigma” of twentieth-century GMSLR, which is that the observed GMSLR has previously been found to exceed the sum of estimated contributions, especially for the earlier decades. The authors propose the following: thermal expansion simulated by climate models may previously have been underestimated because of their not including volcanic forcing in their control state; the rate of glacier mass loss was larger than previously estimated and was not smaller in the first half than in the second half of the century; the Greenland ice sheet could have made a positive contribution throughout the century; and groundwater depletion and reservoir impoundment, which are of opposite sign, may have been approximately equal in magnitude. It is possible to reconstruct the time series of GMSLR from the quantified contributions, apart from a constant residual term, which is small enough to be explained as a long-term contribution from the Antarctic ice sheet. The reconstructions account for the observation that the rate of GMSLR was not much larger during the last 50 years than during the twentieth century as a whole, despite the increasing anthropogenic forcing. Semiempirical methods for projecting GMSLR depend on the existence of a relationship between global climate change and the rate of GMSLR, but the implication of the authors' closure of the budget is that such a relationship is weak or absent during the twentieth century. Article in Journal/Newspaper Antarc* Antarctic glacier Greenland Ice Sheet Northumbria University, Newcastle: Northumbria Research Link (NRL) Antarctic Greenland The Antarctic Journal of Climate 26 13 4476 4499 |
institution |
Open Polar |
collection |
Northumbria University, Newcastle: Northumbria Research Link (NRL) |
op_collection_id |
ftunivnorthumb |
language |
English |
topic |
F800 Physical and Terrestrial Geographical and Environmental Sciences |
spellingShingle |
F800 Physical and Terrestrial Geographical and Environmental Sciences Gregory, Jonathan White, Neil Church, John Bierkens, Marc Box, Jason van den Broeke, Michiel Cogley, Graham Fettweis, Xavier Hanna, Edward Huybrechts, Philippe Konikow, Leonard Leclercq, Paul Marzeion, Ben Oerlemans, Johannes Tamisiea, Mark Wada, Yoshihide Wake, Leanne van de Wal, Roderik Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts? |
topic_facet |
F800 Physical and Terrestrial Geographical and Environmental Sciences |
description |
Confidence in projections of global-mean sea level rise (GMSLR) depends on an ability to account for GMSLR during the twentieth century. There are contributions from ocean thermal expansion, mass loss from glaciers and ice sheets, groundwater extraction, and reservoir impoundment. Progress has been made toward solving the “enigma” of twentieth-century GMSLR, which is that the observed GMSLR has previously been found to exceed the sum of estimated contributions, especially for the earlier decades. The authors propose the following: thermal expansion simulated by climate models may previously have been underestimated because of their not including volcanic forcing in their control state; the rate of glacier mass loss was larger than previously estimated and was not smaller in the first half than in the second half of the century; the Greenland ice sheet could have made a positive contribution throughout the century; and groundwater depletion and reservoir impoundment, which are of opposite sign, may have been approximately equal in magnitude. It is possible to reconstruct the time series of GMSLR from the quantified contributions, apart from a constant residual term, which is small enough to be explained as a long-term contribution from the Antarctic ice sheet. The reconstructions account for the observation that the rate of GMSLR was not much larger during the last 50 years than during the twentieth century as a whole, despite the increasing anthropogenic forcing. Semiempirical methods for projecting GMSLR depend on the existence of a relationship between global climate change and the rate of GMSLR, but the implication of the authors' closure of the budget is that such a relationship is weak or absent during the twentieth century. |
format |
Article in Journal/Newspaper |
author |
Gregory, Jonathan White, Neil Church, John Bierkens, Marc Box, Jason van den Broeke, Michiel Cogley, Graham Fettweis, Xavier Hanna, Edward Huybrechts, Philippe Konikow, Leonard Leclercq, Paul Marzeion, Ben Oerlemans, Johannes Tamisiea, Mark Wada, Yoshihide Wake, Leanne van de Wal, Roderik |
author_facet |
Gregory, Jonathan White, Neil Church, John Bierkens, Marc Box, Jason van den Broeke, Michiel Cogley, Graham Fettweis, Xavier Hanna, Edward Huybrechts, Philippe Konikow, Leonard Leclercq, Paul Marzeion, Ben Oerlemans, Johannes Tamisiea, Mark Wada, Yoshihide Wake, Leanne van de Wal, Roderik |
author_sort |
Gregory, Jonathan |
title |
Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts? |
title_short |
Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts? |
title_full |
Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts? |
title_fullStr |
Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts? |
title_full_unstemmed |
Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts? |
title_sort |
twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts? |
publisher |
American Meteorological Society |
publishDate |
2013 |
url |
https://nrl.northumbria.ac.uk/id/eprint/13070/ https://doi.org/10.1175/JCLI-D-12-00319.1 https://nrl.northumbria.ac.uk/id/eprint/13070/1/leanne_wake_sealevelrise.pdf |
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_relation |
https://nrl.northumbria.ac.uk/id/eprint/13070/1/leanne_wake_sealevelrise.pdf Gregory, Jonathan, White, Neil, Church, John, Bierkens, Marc, Box, Jason, van den Broeke, Michiel, Cogley, Graham, Fettweis, Xavier, Hanna, Edward, Huybrechts, Philippe, Konikow, Leonard, Leclercq, Paul, Marzeion, Ben, Oerlemans, Johannes, Tamisiea, Mark, Wada, Yoshihide, Wake, Leanne and van de Wal, Roderik (2013) Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts? Journal of Climate, 26 (13). pp. 4476-4499. ISSN 0894-8755 |
op_doi |
https://doi.org/10.1175/JCLI-D-12-00319.1 |
container_title |
Journal of Climate |
container_volume |
26 |
container_issue |
13 |
container_start_page |
4476 |
op_container_end_page |
4499 |
_version_ |
1766067055459565568 |