Age models and summer sea surface temperature and winter sea ice concentration for the EPILOG-LGM time slice in the Pacific Southern Ocean
Sea surface temperatures and sea-ice extent are the most critical variables to evaluate the Southern Ocean paleoceanographic evolution in relation to the development of the global carbon cycle, atmospheric CO2 variability and ocean-atmosphere circulation. In contrast to the Atlantic and the Indian s...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.849115 2023-05-15T13:44:47+02:00 Age models and summer sea surface temperature and winter sea ice concentration for the EPILOG-LGM time slice in the Pacific Southern Ocean Benz, Verena Esper, Oliver Gersonde, Rainer Lamy, Frank Tiedemann, Ralf MEDIAN LATITUDE: -58.729754 * MEDIAN LONGITUDE: -142.789862 * SOUTH-BOUND LATITUDE: -63.694330 * WEST-BOUND LONGITUDE: -172.701000 * NORTH-BOUND LATITUDE: -52.812170 * EAST-BOUND LONGITUDE: -107.805500 * DATE/TIME START: 2001-03-19T18:34:00 * DATE/TIME END: 2010-01-17T20:00:00 2016-09-07 application/zip, 29 datasets https://doi.pangaea.de/10.1594/PANGAEA.849115 https://doi.org/10.1594/PANGAEA.849115 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.849115 https://doi.org/10.1594/PANGAEA.849115 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Benz, Verena; Esper, Oliver; Gersonde, Rainer; Lamy, Frank; Tiedemann, Ralf (2016): Last Glacial Maximum sea surface temperature and sea-ice extent in the Pacific sector of the Southern Ocean. Quaternary Science Reviews, 146, 216-237, https://doi.org/10.1016/j.quascirev.2016.06.006 AWI_Paleo Paleoenvironmental Reconstructions from Marine Sediments @ AWI Dataset 2016 ftpangaea https://doi.org/10.1594/PANGAEA.849115 https://doi.org/10.1016/j.quascirev.2016.06.006 2023-01-20T07:33:30Z Sea surface temperatures and sea-ice extent are the most critical variables to evaluate the Southern Ocean paleoceanographic evolution in relation to the development of the global carbon cycle, atmospheric CO2 variability and ocean-atmosphere circulation. In contrast to the Atlantic and the Indian sectors, the Pacific sector of the Southern Ocean has been insufficiently investigated so far. To cover this gap of information we present diatom-based estimates of summer sea surface temperature (SSST) and winter sea-ice concentration (WSI) from 17 sites in the polar South Pacific to study the Last Glacial Maximum (LGM) at the EPILOG time slice (19,000-23,000 cal. years BP). Applied statistical methods are the Imbrie and Kipp Method (IKM) and the Modern Analog Technique (MAT) to estimate temperature and sea-ice concentration, respectively. Our data display a distinct LGM east-west differentiation in SSST and WSI with steeper latitudinal temperature gradients and a winter sea-ice edge located consistently north of the Pacific-Antarctic Ridge in the Ross sea sector. In the eastern sector of our study area, which is governed by the Amundsen Abyssal Plain, the estimates yield weaker latitudinal SSST gradients together with a variable extended winter sea-ice field. In this sector, sea-ice extent may have reached sporadically the area of the present Subantarctic Front at its maximum LGM expansion. This pattern points to topographic forcing as major controller of the frontal system location and sea-ice extent in the western Pacific sector whereas atmospheric conditions like the Southern Annular Mode and the ENSO affected the oceanographic conditions in the eastern Pacific sector. Although it is difficult to depict the location and the physical nature of frontal systems separating the glacial Southern Ocean water masses into different zones, we found a distinct temperature gradient in latitudes straddled by the modern Southern Subtropical Front. Considering that the glacial temperatures north of this zone are similar to the ... Dataset Antarc* Antarctic Ross Sea Sea ice Southern Ocean PANGAEA - Data Publisher for Earth & Environmental Science Antarctic Southern Ocean Ross Sea Pacific Indian Amundsen Abyssal Plain ENVELOPE(-125.000,-125.000,-63.500,-63.500) ENVELOPE(-172.701000,-107.805500,-52.812170,-63.694330) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
AWI_Paleo Paleoenvironmental Reconstructions from Marine Sediments @ AWI |
spellingShingle |
AWI_Paleo Paleoenvironmental Reconstructions from Marine Sediments @ AWI Benz, Verena Esper, Oliver Gersonde, Rainer Lamy, Frank Tiedemann, Ralf Age models and summer sea surface temperature and winter sea ice concentration for the EPILOG-LGM time slice in the Pacific Southern Ocean |
topic_facet |
AWI_Paleo Paleoenvironmental Reconstructions from Marine Sediments @ AWI |
description |
Sea surface temperatures and sea-ice extent are the most critical variables to evaluate the Southern Ocean paleoceanographic evolution in relation to the development of the global carbon cycle, atmospheric CO2 variability and ocean-atmosphere circulation. In contrast to the Atlantic and the Indian sectors, the Pacific sector of the Southern Ocean has been insufficiently investigated so far. To cover this gap of information we present diatom-based estimates of summer sea surface temperature (SSST) and winter sea-ice concentration (WSI) from 17 sites in the polar South Pacific to study the Last Glacial Maximum (LGM) at the EPILOG time slice (19,000-23,000 cal. years BP). Applied statistical methods are the Imbrie and Kipp Method (IKM) and the Modern Analog Technique (MAT) to estimate temperature and sea-ice concentration, respectively. Our data display a distinct LGM east-west differentiation in SSST and WSI with steeper latitudinal temperature gradients and a winter sea-ice edge located consistently north of the Pacific-Antarctic Ridge in the Ross sea sector. In the eastern sector of our study area, which is governed by the Amundsen Abyssal Plain, the estimates yield weaker latitudinal SSST gradients together with a variable extended winter sea-ice field. In this sector, sea-ice extent may have reached sporadically the area of the present Subantarctic Front at its maximum LGM expansion. This pattern points to topographic forcing as major controller of the frontal system location and sea-ice extent in the western Pacific sector whereas atmospheric conditions like the Southern Annular Mode and the ENSO affected the oceanographic conditions in the eastern Pacific sector. Although it is difficult to depict the location and the physical nature of frontal systems separating the glacial Southern Ocean water masses into different zones, we found a distinct temperature gradient in latitudes straddled by the modern Southern Subtropical Front. Considering that the glacial temperatures north of this zone are similar to the ... |
format |
Dataset |
author |
Benz, Verena Esper, Oliver Gersonde, Rainer Lamy, Frank Tiedemann, Ralf |
author_facet |
Benz, Verena Esper, Oliver Gersonde, Rainer Lamy, Frank Tiedemann, Ralf |
author_sort |
Benz, Verena |
title |
Age models and summer sea surface temperature and winter sea ice concentration for the EPILOG-LGM time slice in the Pacific Southern Ocean |
title_short |
Age models and summer sea surface temperature and winter sea ice concentration for the EPILOG-LGM time slice in the Pacific Southern Ocean |
title_full |
Age models and summer sea surface temperature and winter sea ice concentration for the EPILOG-LGM time slice in the Pacific Southern Ocean |
title_fullStr |
Age models and summer sea surface temperature and winter sea ice concentration for the EPILOG-LGM time slice in the Pacific Southern Ocean |
title_full_unstemmed |
Age models and summer sea surface temperature and winter sea ice concentration for the EPILOG-LGM time slice in the Pacific Southern Ocean |
title_sort |
age models and summer sea surface temperature and winter sea ice concentration for the epilog-lgm time slice in the pacific southern ocean |
publisher |
PANGAEA |
publishDate |
2016 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.849115 https://doi.org/10.1594/PANGAEA.849115 |
op_coverage |
MEDIAN LATITUDE: -58.729754 * MEDIAN LONGITUDE: -142.789862 * SOUTH-BOUND LATITUDE: -63.694330 * WEST-BOUND LONGITUDE: -172.701000 * NORTH-BOUND LATITUDE: -52.812170 * EAST-BOUND LONGITUDE: -107.805500 * DATE/TIME START: 2001-03-19T18:34:00 * DATE/TIME END: 2010-01-17T20:00:00 |
long_lat |
ENVELOPE(-125.000,-125.000,-63.500,-63.500) ENVELOPE(-172.701000,-107.805500,-52.812170,-63.694330) |
geographic |
Antarctic Southern Ocean Ross Sea Pacific Indian Amundsen Abyssal Plain |
geographic_facet |
Antarctic Southern Ocean Ross Sea Pacific Indian Amundsen Abyssal Plain |
genre |
Antarc* Antarctic Ross Sea Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctic Ross Sea Sea ice Southern Ocean |
op_source |
Supplement to: Benz, Verena; Esper, Oliver; Gersonde, Rainer; Lamy, Frank; Tiedemann, Ralf (2016): Last Glacial Maximum sea surface temperature and sea-ice extent in the Pacific sector of the Southern Ocean. Quaternary Science Reviews, 146, 216-237, https://doi.org/10.1016/j.quascirev.2016.06.006 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.849115 https://doi.org/10.1594/PANGAEA.849115 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.849115 https://doi.org/10.1016/j.quascirev.2016.06.006 |
_version_ |
1766206341571936256 |