Missing sea-level rise in southeast Greenland during and since the Little Ice Age
The Greenland Ice Sheet has been losing mass at an accelerating rate over the past two decades. Understanding ice mass and glacier changes during the preceding several hundred years, prior to geodetic measurements, is more difficult because evidence of past ice extent in many places was later overri...
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Copernicus Publications
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Online Access: | https://doi.org/10.5194/egusphere-2022-1324 https://noa.gwlb.de/receive/cop_mods_00063822 https://egusphere.copernicus.org/preprints/egusphere-2022-1324/egusphere-2022-1324.pdf |
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00063822 2023-05-15T13:49:22+02:00 Missing sea-level rise in southeast Greenland during and since the Little Ice Age Woodroffe, Sarah Alice Wake, Leanne Mary Kjeldsen, Kristian K. Barlow, Natasha Louise Mary Long, Antony James Kjaer, Kurt Henrik 2022-12 electronic https://doi.org/10.5194/egusphere-2022-1324 https://noa.gwlb.de/receive/cop_mods_00063822 https://egusphere.copernicus.org/preprints/egusphere-2022-1324/egusphere-2022-1324.pdf eng eng Copernicus Publications https://doi.org/10.5194/egusphere-2022-1324 https://noa.gwlb.de/receive/cop_mods_00063822 https://egusphere.copernicus.org/preprints/egusphere-2022-1324/egusphere-2022-1324.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/restrictedAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 2022 ftnonlinearchiv https://doi.org/10.5194/egusphere-2022-1324 2022-12-12T00:12:45Z The Greenland Ice Sheet has been losing mass at an accelerating rate over the past two decades. Understanding ice mass and glacier changes during the preceding several hundred years, prior to geodetic measurements, is more difficult because evidence of past ice extent in many places was later overridden. Saltmarshes provide the only continuous records of Relative Sea Level (RSL) from close to the Greenland Ice Sheet that span the period of time during and since the Little Ice Age (LIA) and can be used to reconstruct ice mass gain and loss over recent centuries. Saltmarsh sediments collected at the mouth of Dronning Marie Dal, close to the Greenland Ice Sheet margin in southeast Greenland, record RSL changes over the past c. 300 years through changing sediment and diatom stratigraphy. These RSL changes record a combination of processes that are dominated by local/regional changes in Greenland Ice Sheet mass balance during this critical period that spans the maximum of the LIA and 20th Century warming. In the early part of the record (1725–1762 CE) the rate of RSL rise is higher than reconstructed from the closest isolation basin at Timmiarmiut, but between 1762–1880 CE the RSL rate is within the error range of rate of RSL change recorded in the isolation basin. RSL begins to slowly fall around 1880 CE and then accelerates since the 1990s, with a total amount of RSL fall of 0.08 ±0.1 m in the last 140 years. Modelled RSL, which takes into account contributions from post-LIA Greenland Ice Sheet Glacio-isostatic Adjustment (GIA), ongoing deglacial GIA, the global non-ice sheet glacial melt fingerprint, contributions from thermosteric effects, the Antarctic mass loss sea-level fingerprint and terrestrial water storage, over-predicts the amount of RSL fall since the end of the LIA by at least 0.5 m. The GIA signal caused by post-LIA Greenland Ice Sheet mass loss is by far the largest contributor to this modelled RSL, and error in its calculation can have a large impact on RSL predictions at Dronning Marie Dal. We ... Article in Journal/Newspaper Antarc* Antarctic glacier Greenland Ice Sheet Niedersächsisches Online-Archiv NOA Antarctic Dronning Marie Dal ENVELOPE(-42.000,-42.000,63.467,63.467) Greenland The Antarctic Timmiarmiut ENVELOPE(-42.217,-42.217,62.533,62.533) |
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Open Polar |
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Niedersächsisches Online-Archiv NOA |
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ftnonlinearchiv |
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English |
topic |
article Verlagsveröffentlichung |
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article Verlagsveröffentlichung Woodroffe, Sarah Alice Wake, Leanne Mary Kjeldsen, Kristian K. Barlow, Natasha Louise Mary Long, Antony James Kjaer, Kurt Henrik Missing sea-level rise in southeast Greenland during and since the Little Ice Age |
topic_facet |
article Verlagsveröffentlichung |
description |
The Greenland Ice Sheet has been losing mass at an accelerating rate over the past two decades. Understanding ice mass and glacier changes during the preceding several hundred years, prior to geodetic measurements, is more difficult because evidence of past ice extent in many places was later overridden. Saltmarshes provide the only continuous records of Relative Sea Level (RSL) from close to the Greenland Ice Sheet that span the period of time during and since the Little Ice Age (LIA) and can be used to reconstruct ice mass gain and loss over recent centuries. Saltmarsh sediments collected at the mouth of Dronning Marie Dal, close to the Greenland Ice Sheet margin in southeast Greenland, record RSL changes over the past c. 300 years through changing sediment and diatom stratigraphy. These RSL changes record a combination of processes that are dominated by local/regional changes in Greenland Ice Sheet mass balance during this critical period that spans the maximum of the LIA and 20th Century warming. In the early part of the record (1725–1762 CE) the rate of RSL rise is higher than reconstructed from the closest isolation basin at Timmiarmiut, but between 1762–1880 CE the RSL rate is within the error range of rate of RSL change recorded in the isolation basin. RSL begins to slowly fall around 1880 CE and then accelerates since the 1990s, with a total amount of RSL fall of 0.08 ±0.1 m in the last 140 years. Modelled RSL, which takes into account contributions from post-LIA Greenland Ice Sheet Glacio-isostatic Adjustment (GIA), ongoing deglacial GIA, the global non-ice sheet glacial melt fingerprint, contributions from thermosteric effects, the Antarctic mass loss sea-level fingerprint and terrestrial water storage, over-predicts the amount of RSL fall since the end of the LIA by at least 0.5 m. The GIA signal caused by post-LIA Greenland Ice Sheet mass loss is by far the largest contributor to this modelled RSL, and error in its calculation can have a large impact on RSL predictions at Dronning Marie Dal. We ... |
format |
Article in Journal/Newspaper |
author |
Woodroffe, Sarah Alice Wake, Leanne Mary Kjeldsen, Kristian K. Barlow, Natasha Louise Mary Long, Antony James Kjaer, Kurt Henrik |
author_facet |
Woodroffe, Sarah Alice Wake, Leanne Mary Kjeldsen, Kristian K. Barlow, Natasha Louise Mary Long, Antony James Kjaer, Kurt Henrik |
author_sort |
Woodroffe, Sarah Alice |
title |
Missing sea-level rise in southeast Greenland during and since the Little Ice Age |
title_short |
Missing sea-level rise in southeast Greenland during and since the Little Ice Age |
title_full |
Missing sea-level rise in southeast Greenland during and since the Little Ice Age |
title_fullStr |
Missing sea-level rise in southeast Greenland during and since the Little Ice Age |
title_full_unstemmed |
Missing sea-level rise in southeast Greenland during and since the Little Ice Age |
title_sort |
missing sea-level rise in southeast greenland during and since the little ice age |
publisher |
Copernicus Publications |
publishDate |
2022 |
url |
https://doi.org/10.5194/egusphere-2022-1324 https://noa.gwlb.de/receive/cop_mods_00063822 https://egusphere.copernicus.org/preprints/egusphere-2022-1324/egusphere-2022-1324.pdf |
long_lat |
ENVELOPE(-42.000,-42.000,63.467,63.467) ENVELOPE(-42.217,-42.217,62.533,62.533) |
geographic |
Antarctic Dronning Marie Dal Greenland The Antarctic Timmiarmiut |
geographic_facet |
Antarctic Dronning Marie Dal Greenland The Antarctic Timmiarmiut |
genre |
Antarc* Antarctic glacier Greenland Ice Sheet |
genre_facet |
Antarc* Antarctic glacier Greenland Ice Sheet |
op_relation |
https://doi.org/10.5194/egusphere-2022-1324 https://noa.gwlb.de/receive/cop_mods_00063822 https://egusphere.copernicus.org/preprints/egusphere-2022-1324/egusphere-2022-1324.pdf |
op_rights |
https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/restrictedAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5194/egusphere-2022-1324 |
_version_ |
1766251246321139712 |