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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 Open Access
Language:en
Published: PANGAEA 2023
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.955733
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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 Agulha Leakage. Changes in the surface hydrography of the Indian Ocean may therefore impact on the global overturning circulation. Here we present spectral, and cross spectral analysis results which show that Indian Ocean surface salinity and temperature increased during glacial intensification, with a significant lag prior to deglaciations.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_955733
institution PANGAEA
language en
publishDate 2023
publisher PANGAEA
record_format pangaea
spellingShingle Spectral and Cross Spectral Analysis for IODP Site 361-U1476 SST and planktic d18Osw-ivc
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
Calculated; Indian Ocean; oxygen isotope ratios; Oxygen isotopes; planktic foraminifera; Salinity; Temperature; Sea surface salinity; Sea surface temperature; Spectral coherence; Spectral cycle frequency; Spectral density; Spectral period; Spectral phase
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. Here we present spectral, and cross spectral analysis results which show that Indian Ocean surface salinity and temperature increased during glacial intensification, with a significant lag prior to deglaciations.
title Spectral and Cross Spectral Analysis for IODP Site 361-U1476 SST and planktic d18Osw-ivc
topic Calculated; Indian Ocean; oxygen isotope ratios; Oxygen isotopes; planktic foraminifera; Salinity; Temperature; Sea surface salinity; Sea surface temperature; Spectral coherence; Spectral cycle frequency; Spectral density; Spectral period; Spectral phase
url https://doi.org/10.1594/PANGAEA.955733