Ice sheet model-derived global mean sea level and whole ocean oxygen isotopes
Indian Ocean surface circulation is an important part of the global ocean conveyor belt, and is connected via two important gateways including the Indonesian Throughflow, and the Agulha Leakage. Changes in the surface hydrography of the Indian Ocean may therefore impact on the global overturning cir...
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2023
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.955711 https://doi.org/10.1594/PANGAEA.955711 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.955711 2024-09-15T18:12:13+00:00 Ice sheet model-derived global mean sea level and whole ocean oxygen isotopes Nuber, Sophie Rae, James W B Zhang, Xu Andersen, Morten L Dumont, Matthew Mithan, T Huw Sun, Yuchen de Boer, Bas Hall, Ian R Barker, Stephen 2023 text/tab-separated-values, 2800 data points https://doi.pangaea.de/10.1594/PANGAEA.955711 https://doi.org/10.1594/PANGAEA.955711 en eng PANGAEA https://doi.org/10.1594/PANGAEA.955609 https://doi.pangaea.de/10.1594/PANGAEA.955711 https://doi.org/10.1594/PANGAEA.955711 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess AGE Global mean sea level Ice sheet-topography model ANICE-SELEN Indian Ocean oxygen isotope ratios oxygen isotopes planktic foraminifera Salinity Temperature Sea surface salinity Sea surface temperature δ18O ice volume effect dataset 2023 ftpangaea https://doi.org/10.1594/PANGAEA.95571110.1594/PANGAEA.955609 2024-07-24T02:31:43Z Indian Ocean surface circulation is an important part of the global ocean conveyor belt, and is connected via two important gateways including the Indonesian Throughflow, and the Agulha Leakage. Changes in the surface hydrography of the Indian Ocean may therefore impact on the global overturning circulation. Using planktonic foraminifera-based reconstructions of Indian Ocean surface salinity and temperature, we find that Indian Ocean surface water salinify during glacial intensification. Here we present reconstructions of global mean sea level using the ice sheet model ANICE and benthic foraminifera oxygen isotope data from U1476 to analyse changes in mean global sea level and calculate whole ocean changes in seawater oxygen isotopes. We use this information to show that the Indian Ocean surface hydrography changed in different ways from other ocean basins during Late Pleistocene glacial-interglacial cycles. Dataset Ice Sheet Planktonic foraminifera PANGAEA - Data Publisher for Earth & Environmental Science |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
AGE Global mean sea level Ice sheet-topography model ANICE-SELEN Indian Ocean oxygen isotope ratios oxygen isotopes planktic foraminifera Salinity Temperature Sea surface salinity Sea surface temperature δ18O ice volume effect |
spellingShingle |
AGE Global mean sea level Ice sheet-topography model ANICE-SELEN Indian Ocean oxygen isotope ratios oxygen isotopes planktic foraminifera Salinity Temperature Sea surface salinity Sea surface temperature δ18O ice volume effect Nuber, Sophie Rae, James W B Zhang, Xu Andersen, Morten L Dumont, Matthew Mithan, T Huw Sun, Yuchen de Boer, Bas Hall, Ian R Barker, Stephen Ice sheet model-derived global mean sea level and whole ocean oxygen isotopes |
topic_facet |
AGE Global mean sea level Ice sheet-topography model ANICE-SELEN Indian Ocean oxygen isotope ratios oxygen isotopes planktic foraminifera Salinity Temperature Sea surface salinity Sea surface temperature δ18O ice volume effect |
description |
Indian Ocean surface circulation is an important part of the global ocean conveyor belt, and is connected via two important gateways including the Indonesian Throughflow, and the Agulha Leakage. Changes in the surface hydrography of the Indian Ocean may therefore impact on the global overturning circulation. Using planktonic foraminifera-based reconstructions of Indian Ocean surface salinity and temperature, we find that Indian Ocean surface water salinify during glacial intensification. Here we present reconstructions of global mean sea level using the ice sheet model ANICE and benthic foraminifera oxygen isotope data from U1476 to analyse changes in mean global sea level and calculate whole ocean changes in seawater oxygen isotopes. We use this information to show that the Indian Ocean surface hydrography changed in different ways from other ocean basins during Late Pleistocene glacial-interglacial cycles. |
format |
Dataset |
author |
Nuber, Sophie Rae, James W B Zhang, Xu Andersen, Morten L Dumont, Matthew Mithan, T Huw Sun, Yuchen de Boer, Bas Hall, Ian R Barker, Stephen |
author_facet |
Nuber, Sophie Rae, James W B Zhang, Xu Andersen, Morten L Dumont, Matthew Mithan, T Huw Sun, Yuchen de Boer, Bas Hall, Ian R Barker, Stephen |
author_sort |
Nuber, Sophie |
title |
Ice sheet model-derived global mean sea level and whole ocean oxygen isotopes |
title_short |
Ice sheet model-derived global mean sea level and whole ocean oxygen isotopes |
title_full |
Ice sheet model-derived global mean sea level and whole ocean oxygen isotopes |
title_fullStr |
Ice sheet model-derived global mean sea level and whole ocean oxygen isotopes |
title_full_unstemmed |
Ice sheet model-derived global mean sea level and whole ocean oxygen isotopes |
title_sort |
ice sheet model-derived global mean sea level and whole ocean oxygen isotopes |
publisher |
PANGAEA |
publishDate |
2023 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.955711 https://doi.org/10.1594/PANGAEA.955711 |
genre |
Ice Sheet Planktonic foraminifera |
genre_facet |
Ice Sheet Planktonic foraminifera |
op_relation |
https://doi.org/10.1594/PANGAEA.955609 https://doi.pangaea.de/10.1594/PANGAEA.955711 https://doi.org/10.1594/PANGAEA.955711 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.95571110.1594/PANGAEA.955609 |
_version_ |
1810449800100839424 |