Sea surface temperature in the Indian sector of the Southern Ocean over the Late Glacial and Holocene
Centennial- and millennial-scale variability of Southern Ocean temperature over the Holocene is poorly known, due to both short instrumental records and sparsely distributed high-resolution temperature reconstructions, with evidence for past temperature variations in the region coming mainly from ic...
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fttriple:oai:gotriple.eu:GZEGu6t5q6Y4SUpw8m_k4 2023-05-15T16:39:18+02:00 Sea surface temperature in the Indian sector of the Southern Ocean over the Late Glacial and Holocene Orme, Lisa Claire Crosta, Xavier Miettinen, Arto Divine, Dmitry V. Husum, Katrine Isaksson, Elisabeth Wacker, Lukas Mohan, Rahul Ther, Olivier Ikehara, Minoru 2020-08-07 https://doi.org/10.5194/cp-16-1451-2020 https://cp.copernicus.org/articles/16/1451/2020/ en eng Copernicus Publications doi:10.5194/cp-16-1451-2020 10670/1.o3qapm 1814-9324 1814-9332 https://cp.copernicus.org/articles/16/1451/2020/ undefined Geographica Helvetica - geography eISSN: 1814-9332 envir geo Text https://vocabularies.coar-repositories.org/resource_types/c_18cf/ Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2020 fttriple https://doi.org/10.5194/cp-16-1451-2020 2023-01-22T17:39:04Z Centennial- and millennial-scale variability of Southern Ocean temperature over the Holocene is poorly known, due to both short instrumental records and sparsely distributed high-resolution temperature reconstructions, with evidence for past temperature variations in the region coming mainly from ice core records. Here we present a high-resolution (∼60 year), diatom-based sea surface temperature (SST) reconstruction from the western Indian sector of the Southern Ocean that spans the interval 14.2 to 1.0 ka (calibrated kiloyears before present). During the late deglaciation, the new SST record shows cool temperatures at 14.2–12.9 ka and gradual warming between 12.9 and 11.6 ka in phase with atmospheric temperature evolution. This supports the evolution of the Southern Ocean SST during the deglaciation being linked with a complex combination of processes and drivers associated with reorganisations of atmospheric and oceanic circulation patterns. Specifically, we suggest that Southern Ocean surface warming coincided, within the dating uncertainties, with the reconstructed slowdown of the Atlantic Meridional Overturning Circulation (AMOC), rising atmospheric CO2 levels, changes in the southern westerly winds and enhanced upwelling. During the Holocene the record shows warm and stable temperatures from 11.6 to 8.7 ka followed by a slight cooling and greater variability from 8.7 to 1 ka, with a quasi-periodic variability of 200–260 years identified by spectral analysis. We suggest that the increased variability during the mid- to late Holocene reflects the establishment of centennial variability in SST connected with changes in the high-latitude atmospheric circulation and Southern Ocean convection. Article in Journal/Newspaper ice core Southern Ocean Unknown Southern Ocean Indian Climate of the Past 16 4 1451 1467 |
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envir geo Orme, Lisa Claire Crosta, Xavier Miettinen, Arto Divine, Dmitry V. Husum, Katrine Isaksson, Elisabeth Wacker, Lukas Mohan, Rahul Ther, Olivier Ikehara, Minoru Sea surface temperature in the Indian sector of the Southern Ocean over the Late Glacial and Holocene |
topic_facet |
envir geo |
description |
Centennial- and millennial-scale variability of Southern Ocean temperature over the Holocene is poorly known, due to both short instrumental records and sparsely distributed high-resolution temperature reconstructions, with evidence for past temperature variations in the region coming mainly from ice core records. Here we present a high-resolution (∼60 year), diatom-based sea surface temperature (SST) reconstruction from the western Indian sector of the Southern Ocean that spans the interval 14.2 to 1.0 ka (calibrated kiloyears before present). During the late deglaciation, the new SST record shows cool temperatures at 14.2–12.9 ka and gradual warming between 12.9 and 11.6 ka in phase with atmospheric temperature evolution. This supports the evolution of the Southern Ocean SST during the deglaciation being linked with a complex combination of processes and drivers associated with reorganisations of atmospheric and oceanic circulation patterns. Specifically, we suggest that Southern Ocean surface warming coincided, within the dating uncertainties, with the reconstructed slowdown of the Atlantic Meridional Overturning Circulation (AMOC), rising atmospheric CO2 levels, changes in the southern westerly winds and enhanced upwelling. During the Holocene the record shows warm and stable temperatures from 11.6 to 8.7 ka followed by a slight cooling and greater variability from 8.7 to 1 ka, with a quasi-periodic variability of 200–260 years identified by spectral analysis. We suggest that the increased variability during the mid- to late Holocene reflects the establishment of centennial variability in SST connected with changes in the high-latitude atmospheric circulation and Southern Ocean convection. |
format |
Article in Journal/Newspaper |
author |
Orme, Lisa Claire Crosta, Xavier Miettinen, Arto Divine, Dmitry V. Husum, Katrine Isaksson, Elisabeth Wacker, Lukas Mohan, Rahul Ther, Olivier Ikehara, Minoru |
author_facet |
Orme, Lisa Claire Crosta, Xavier Miettinen, Arto Divine, Dmitry V. Husum, Katrine Isaksson, Elisabeth Wacker, Lukas Mohan, Rahul Ther, Olivier Ikehara, Minoru |
author_sort |
Orme, Lisa Claire |
title |
Sea surface temperature in the Indian sector of the Southern Ocean over the Late Glacial and Holocene |
title_short |
Sea surface temperature in the Indian sector of the Southern Ocean over the Late Glacial and Holocene |
title_full |
Sea surface temperature in the Indian sector of the Southern Ocean over the Late Glacial and Holocene |
title_fullStr |
Sea surface temperature in the Indian sector of the Southern Ocean over the Late Glacial and Holocene |
title_full_unstemmed |
Sea surface temperature in the Indian sector of the Southern Ocean over the Late Glacial and Holocene |
title_sort |
sea surface temperature in the indian sector of the southern ocean over the late glacial and holocene |
publisher |
Copernicus Publications |
publishDate |
2020 |
url |
https://doi.org/10.5194/cp-16-1451-2020 https://cp.copernicus.org/articles/16/1451/2020/ |
geographic |
Southern Ocean Indian |
geographic_facet |
Southern Ocean Indian |
genre |
ice core Southern Ocean |
genre_facet |
ice core Southern Ocean |
op_source |
Geographica Helvetica - geography eISSN: 1814-9332 |
op_relation |
doi:10.5194/cp-16-1451-2020 10670/1.o3qapm 1814-9324 1814-9332 https://cp.copernicus.org/articles/16/1451/2020/ |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/cp-16-1451-2020 |
container_title |
Climate of the Past |
container_volume |
16 |
container_issue |
4 |
container_start_page |
1451 |
op_container_end_page |
1467 |
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1766029634630057984 |