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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Bibliographic Details
Main Authors: 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
Format: Dataset
Language:English
Published: PANGAEA 2023
Subjects:
AGE
Online Access:https://dx.doi.org/10.1594/pangaea.955720
https://doi.pangaea.de/10.1594/PANGAEA.955720
id ftdatacite:10.1594/pangaea.955720
record_format openpolar
spelling ftdatacite:10.1594/pangaea.955720 2024-09-15T18:12:24+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 https://dx.doi.org/10.1594/pangaea.955720 https://doi.pangaea.de/10.1594/PANGAEA.955720 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.955609 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Indian Ocean oxygen isotope ratios oxygen isotopes planktic foraminifera Salinity; Temperature Sea surface salinity Sea surface temperature Global mean sea level AGE Ratio Calculated Calculated from Ice sheet-topography model, ANICE-SELEN modelled dataset Dataset 2023 ftdatacite https://doi.org/10.1594/pangaea.95572010.1594/pangaea.955609 2024-08-01T10:54:59Z 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 DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Indian Ocean
oxygen isotope ratios
oxygen isotopes
planktic foraminifera
Salinity; Temperature
Sea surface salinity
Sea surface temperature
Global mean sea level
AGE
Ratio
Calculated
Calculated from Ice sheet-topography model, ANICE-SELEN
modelled
spellingShingle Indian Ocean
oxygen isotope ratios
oxygen isotopes
planktic foraminifera
Salinity; Temperature
Sea surface salinity
Sea surface temperature
Global mean sea level
AGE
Ratio
Calculated
Calculated from Ice sheet-topography model, ANICE-SELEN
modelled
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 Indian Ocean
oxygen isotope ratios
oxygen isotopes
planktic foraminifera
Salinity; Temperature
Sea surface salinity
Sea surface temperature
Global mean sea level
AGE
Ratio
Calculated
Calculated from Ice sheet-topography model, ANICE-SELEN
modelled
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://dx.doi.org/10.1594/pangaea.955720
https://doi.pangaea.de/10.1594/PANGAEA.955720
genre Ice Sheet
Planktonic foraminifera
genre_facet Ice Sheet
Planktonic foraminifera
op_relation https://dx.doi.org/10.1594/pangaea.955609
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.95572010.1594/pangaea.955609
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