Common millennial-scale variability of Antarctic and southern ocean temperatures during the past 5000 years reconstructed from the EPICA Dome C ice core
Measurements of the two water stable isotopes (dD and d18O) along EPICA (European Project for Ice Coring in Antarctica) Dome C ice core are combined with simple isotopic modelling (distillation models) to reconstruct the variability of both the site temperature (East Antarctica) and the moisture sou...
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Online Access: | http://hdl.handle.net/11368/2626852 https://doi.org/10.1191/0959683604hl697ft |
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ftunitriestiris:oai:arts.units.it:11368/2626852 2023-05-15T13:53:04+02:00 Common millennial-scale variability of Antarctic and southern ocean temperatures during the past 5000 years reconstructed from the EPICA Dome C ice core Masson Delmotte V. Jouzel J. STENNI, BARBARA Masson Delmotte, V. Stenni, Barbara Jouzel, J. 2004 http://hdl.handle.net/11368/2626852 https://doi.org/10.1191/0959683604hl697ft eng eng volume:14 issue:2 firstpage:145 lastpage:151 numberofpages:7 journal:THE HOLOCENE http://hdl.handle.net/11368/2626852 doi:10.1191/0959683604hl697ft info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-0346682032 Millennial-scale variability climatic variation ice core EPICA Southern Ocean Dome C isotopic modelling Climatic Optimum Holocene Antarctica info:eu-repo/semantics/article 2004 ftunitriestiris https://doi.org/10.1191/0959683604hl697ft 2023-04-09T06:11:12Z Measurements of the two water stable isotopes (dD and d18O) along EPICA (European Project for Ice Coring in Antarctica) Dome C ice core are combined with simple isotopic modelling (distillation models) to reconstruct the variability of both the site temperature (East Antarctica) and the moisture source temperature (nowadays probably the subantarctic Indian Ocean). We discuss the difference between the reconstructed site and source temperature profiles with respect to the initial isotopic data. We show that (i) the early Holocene optimum appears first in Antarctica and 800 years later in the Southern Ocean, and (ii) during the last 5000 years, the site and source temperatures co-vary at the centennial timescale. An 833-year periodicity is observed only on deuterium and site temperature and therefore probably of local origin. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica EPICA ice core Southern Ocean Università degli studi di Trieste: ArTS (Archivio della ricerca di Trieste) Antarctic Southern Ocean East Antarctica Indian The Holocene 14 2 145 151 |
institution |
Open Polar |
collection |
Università degli studi di Trieste: ArTS (Archivio della ricerca di Trieste) |
op_collection_id |
ftunitriestiris |
language |
English |
topic |
Millennial-scale variability climatic variation ice core EPICA Southern Ocean Dome C isotopic modelling Climatic Optimum Holocene Antarctica |
spellingShingle |
Millennial-scale variability climatic variation ice core EPICA Southern Ocean Dome C isotopic modelling Climatic Optimum Holocene Antarctica Masson Delmotte V. Jouzel J. STENNI, BARBARA Common millennial-scale variability of Antarctic and southern ocean temperatures during the past 5000 years reconstructed from the EPICA Dome C ice core |
topic_facet |
Millennial-scale variability climatic variation ice core EPICA Southern Ocean Dome C isotopic modelling Climatic Optimum Holocene Antarctica |
description |
Measurements of the two water stable isotopes (dD and d18O) along EPICA (European Project for Ice Coring in Antarctica) Dome C ice core are combined with simple isotopic modelling (distillation models) to reconstruct the variability of both the site temperature (East Antarctica) and the moisture source temperature (nowadays probably the subantarctic Indian Ocean). We discuss the difference between the reconstructed site and source temperature profiles with respect to the initial isotopic data. We show that (i) the early Holocene optimum appears first in Antarctica and 800 years later in the Southern Ocean, and (ii) during the last 5000 years, the site and source temperatures co-vary at the centennial timescale. An 833-year periodicity is observed only on deuterium and site temperature and therefore probably of local origin. |
author2 |
Masson Delmotte, V. Stenni, Barbara Jouzel, J. |
format |
Article in Journal/Newspaper |
author |
Masson Delmotte V. Jouzel J. STENNI, BARBARA |
author_facet |
Masson Delmotte V. Jouzel J. STENNI, BARBARA |
author_sort |
Masson Delmotte V. |
title |
Common millennial-scale variability of Antarctic and southern ocean temperatures during the past 5000 years reconstructed from the EPICA Dome C ice core |
title_short |
Common millennial-scale variability of Antarctic and southern ocean temperatures during the past 5000 years reconstructed from the EPICA Dome C ice core |
title_full |
Common millennial-scale variability of Antarctic and southern ocean temperatures during the past 5000 years reconstructed from the EPICA Dome C ice core |
title_fullStr |
Common millennial-scale variability of Antarctic and southern ocean temperatures during the past 5000 years reconstructed from the EPICA Dome C ice core |
title_full_unstemmed |
Common millennial-scale variability of Antarctic and southern ocean temperatures during the past 5000 years reconstructed from the EPICA Dome C ice core |
title_sort |
common millennial-scale variability of antarctic and southern ocean temperatures during the past 5000 years reconstructed from the epica dome c ice core |
publishDate |
2004 |
url |
http://hdl.handle.net/11368/2626852 https://doi.org/10.1191/0959683604hl697ft |
geographic |
Antarctic Southern Ocean East Antarctica Indian |
geographic_facet |
Antarctic Southern Ocean East Antarctica Indian |
genre |
Antarc* Antarctic Antarctica East Antarctica EPICA ice core Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctica East Antarctica EPICA ice core Southern Ocean |
op_relation |
volume:14 issue:2 firstpage:145 lastpage:151 numberofpages:7 journal:THE HOLOCENE http://hdl.handle.net/11368/2626852 doi:10.1191/0959683604hl697ft info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-0346682032 |
op_doi |
https://doi.org/10.1191/0959683604hl697ft |
container_title |
The Holocene |
container_volume |
14 |
container_issue |
2 |
container_start_page |
145 |
op_container_end_page |
151 |
_version_ |
1766258027249270784 |