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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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://doi.pangaea.de/10.1594/PANGAEA.955711
https://doi.org/10.1594/PANGAEA.955711
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.955711
record_format openpolar
spelling 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