Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial
Coinciding with global warming, Arctic sea ice has rapidly decreased during the last four decades and climate scenarios suggest that sea ice may completely disappear during summer within the next about 50-100 years. Here we produce Arctic sea ice biomarker proxy records for the penultimate glacial (...
Published in: | Nature Communications |
---|---|
Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Nature Publishing Group
2017
|
Subjects: | |
Online Access: | https://archimer.ifremer.fr/doc/00495/60712/65326.pdf https://archimer.ifremer.fr/doc/00495/60712/65327.pdf https://archimer.ifremer.fr/doc/00495/60712/65340.pdf https://doi.org/10.1038/s41467-017-00552-1 https://archimer.ifremer.fr/doc/00495/60712/ |
id |
ftarchimer:oai:archimer.ifremer.fr:60712 |
---|---|
record_format |
openpolar |
spelling |
ftarchimer:oai:archimer.ifremer.fr:60712 2023-05-15T14:37:42+02:00 Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial Stein, Ruediger Fahl, Kirsten Gierz, Paul Niessen, Frank Lohmann, Gerrit 2017-08 application/pdf https://archimer.ifremer.fr/doc/00495/60712/65326.pdf https://archimer.ifremer.fr/doc/00495/60712/65327.pdf https://archimer.ifremer.fr/doc/00495/60712/65340.pdf https://doi.org/10.1038/s41467-017-00552-1 https://archimer.ifremer.fr/doc/00495/60712/ eng eng Nature Publishing Group https://archimer.ifremer.fr/doc/00495/60712/65326.pdf https://archimer.ifremer.fr/doc/00495/60712/65327.pdf https://archimer.ifremer.fr/doc/00495/60712/65340.pdf doi:10.1038/s41467-017-00552-1 https://archimer.ifremer.fr/doc/00495/60712/ info:eu-repo/semantics/openAccess restricted use Nature Communications (2041-1723) (Nature Publishing Group), 2017-08 , Vol. 8 , N. 373 , P. 13p. text Publication info:eu-repo/semantics/article 2017 ftarchimer https://doi.org/10.1038/s41467-017-00552-1 2021-09-23T20:32:46Z Coinciding with global warming, Arctic sea ice has rapidly decreased during the last four decades and climate scenarios suggest that sea ice may completely disappear during summer within the next about 50-100 years. Here we produce Arctic sea ice biomarker proxy records for the penultimate glacial (Marine Isotope Stage 6) and the subsequent last interglacial (Marine Isotope Stage 5e). The latter is a time interval when the high latitudes were significantly warmer than today. We document that even under such warmer climate conditions, sea ice existed in the central Arctic Ocean during summer, whereas sea ice was significantly reduced along the Barents Sea continental margin influenced by Atlantic Water inflow. Our proxy reconstruction of the last interglacial sea ice cover is supported by climate simulations, although some proxy data/model inconsistencies still exist. During late Marine Isotope Stage 6, polynya-type conditions occurred off the major ice sheets along the northern Barents and East Siberian continental margins, contradicting a giant Marine Isotope Stage 6 ice shelf that covered the entire Arctic Ocean. Article in Journal/Newspaper Arctic Arctic Ocean Barents Sea Global warming Ice Shelf Sea ice Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Arctic Arctic Ocean Barents Sea Nature Communications 8 1 |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
description |
Coinciding with global warming, Arctic sea ice has rapidly decreased during the last four decades and climate scenarios suggest that sea ice may completely disappear during summer within the next about 50-100 years. Here we produce Arctic sea ice biomarker proxy records for the penultimate glacial (Marine Isotope Stage 6) and the subsequent last interglacial (Marine Isotope Stage 5e). The latter is a time interval when the high latitudes were significantly warmer than today. We document that even under such warmer climate conditions, sea ice existed in the central Arctic Ocean during summer, whereas sea ice was significantly reduced along the Barents Sea continental margin influenced by Atlantic Water inflow. Our proxy reconstruction of the last interglacial sea ice cover is supported by climate simulations, although some proxy data/model inconsistencies still exist. During late Marine Isotope Stage 6, polynya-type conditions occurred off the major ice sheets along the northern Barents and East Siberian continental margins, contradicting a giant Marine Isotope Stage 6 ice shelf that covered the entire Arctic Ocean. |
format |
Article in Journal/Newspaper |
author |
Stein, Ruediger Fahl, Kirsten Gierz, Paul Niessen, Frank Lohmann, Gerrit |
spellingShingle |
Stein, Ruediger Fahl, Kirsten Gierz, Paul Niessen, Frank Lohmann, Gerrit Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial |
author_facet |
Stein, Ruediger Fahl, Kirsten Gierz, Paul Niessen, Frank Lohmann, Gerrit |
author_sort |
Stein, Ruediger |
title |
Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial |
title_short |
Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial |
title_full |
Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial |
title_fullStr |
Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial |
title_full_unstemmed |
Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial |
title_sort |
arctic ocean sea ice cover during the penultimate glacial and the last interglacial |
publisher |
Nature Publishing Group |
publishDate |
2017 |
url |
https://archimer.ifremer.fr/doc/00495/60712/65326.pdf https://archimer.ifremer.fr/doc/00495/60712/65327.pdf https://archimer.ifremer.fr/doc/00495/60712/65340.pdf https://doi.org/10.1038/s41467-017-00552-1 https://archimer.ifremer.fr/doc/00495/60712/ |
geographic |
Arctic Arctic Ocean Barents Sea |
geographic_facet |
Arctic Arctic Ocean Barents Sea |
genre |
Arctic Arctic Ocean Barents Sea Global warming Ice Shelf Sea ice |
genre_facet |
Arctic Arctic Ocean Barents Sea Global warming Ice Shelf Sea ice |
op_source |
Nature Communications (2041-1723) (Nature Publishing Group), 2017-08 , Vol. 8 , N. 373 , P. 13p. |
op_relation |
https://archimer.ifremer.fr/doc/00495/60712/65326.pdf https://archimer.ifremer.fr/doc/00495/60712/65327.pdf https://archimer.ifremer.fr/doc/00495/60712/65340.pdf doi:10.1038/s41467-017-00552-1 https://archimer.ifremer.fr/doc/00495/60712/ |
op_rights |
info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1038/s41467-017-00552-1 |
container_title |
Nature Communications |
container_volume |
8 |
container_issue |
1 |
_version_ |
1766309911153606656 |