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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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://doi.pangaea.de/10.1594/PANGAEA.955720
https://doi.org/10.1594/PANGAEA.955720
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.955720
record_format openpolar
spelling 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