ANICE-SELEN topography model changes in land to sea ratios in the Indonesian Archipelago
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 Agulhas Leakage. Changes in the surface hydrography of the Indian Ocean may therefore impact on the global overturning ci...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.955720 2024-09-15T18:12:23+00:00 ANICE-SELEN topography model changes in land to sea ratios in the Indonesian Archipelago 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, 1614 data points https://doi.pangaea.de/10.1594/PANGAEA.955720 https://doi.org/10.1594/PANGAEA.955720 en eng PANGAEA https://doi.org/10.1594/PANGAEA.955609 https://doi.pangaea.de/10.1594/PANGAEA.955720 https://doi.org/10.1594/PANGAEA.955720 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess AGE Calculated Calculated from Ice sheet-topography model ANICE-SELEN Global mean sea level Indian Ocean modelled oxygen isotope ratios oxygen isotopes planktic foraminifera Ratio Salinity Temperature Sea surface salinity Sea surface temperature dataset 2023 ftpangaea https://doi.org/10.1594/PANGAEA.95572010.1594/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 Agulhas 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 became saliter during glacial intensification. Here we present bathymetrical change data for the Indonesian Archipelago which shows that the Indonesian Throughflow was likely impacted due to changes in global mean sea level and possibly drove the changes in salinity during a glacial cycle. 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 Calculated Calculated from Ice sheet-topography model ANICE-SELEN Global mean sea level Indian Ocean modelled oxygen isotope ratios oxygen isotopes planktic foraminifera Ratio Salinity Temperature Sea surface salinity Sea surface temperature |
spellingShingle |
AGE Calculated Calculated from Ice sheet-topography model ANICE-SELEN Global mean sea level Indian Ocean modelled oxygen isotope ratios oxygen isotopes planktic foraminifera Ratio Salinity Temperature Sea surface salinity Sea surface temperature 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 ANICE-SELEN topography model changes in land to sea ratios in the Indonesian Archipelago |
topic_facet |
AGE Calculated Calculated from Ice sheet-topography model ANICE-SELEN Global mean sea level Indian Ocean modelled oxygen isotope ratios oxygen isotopes planktic foraminifera Ratio Salinity Temperature Sea surface salinity Sea surface temperature |
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 Agulhas 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 became saliter during glacial intensification. Here we present bathymetrical change data for the Indonesian Archipelago which shows that the Indonesian Throughflow was likely impacted due to changes in global mean sea level and possibly drove the changes in salinity during a glacial cycle. |
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 |
ANICE-SELEN topography model changes in land to sea ratios in the Indonesian Archipelago |
title_short |
ANICE-SELEN topography model changes in land to sea ratios in the Indonesian Archipelago |
title_full |
ANICE-SELEN topography model changes in land to sea ratios in the Indonesian Archipelago |
title_fullStr |
ANICE-SELEN topography model changes in land to sea ratios in the Indonesian Archipelago |
title_full_unstemmed |
ANICE-SELEN topography model changes in land to sea ratios in the Indonesian Archipelago |
title_sort |
anice-selen topography model changes in land to sea ratios in the indonesian archipelago |
publisher |
PANGAEA |
publishDate |
2023 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.955720 https://doi.org/10.1594/PANGAEA.955720 |
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.955720 https://doi.org/10.1594/PANGAEA.955720 |
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.95572010.1594/PANGAEA.955609 |
_version_ |
1810449975568498688 |