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Auteurs principaux: 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 Open Access
Langue:en
Publié: PANGAEA 2023
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Accès en ligne:https://doi.org/10.1594/PANGAEA.955720
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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
collection Datos científicos de ciencias marinas y ambientales
contents 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 Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_955720
institution PANGAEA
language en
publishDate 2023
publisher PANGAEA
record_format pangaea
spellingShingle 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
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
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.
title ANICE-SELEN topography model changes in land to sea ratios in the Indonesian Archipelago
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
url https://doi.org/10.1594/PANGAEA.955720