Decadal variability of sea surface temperatures off North Iceland over the last 2000 years

International audience Ocean variability at decadal time-scales remains poorly described partly because of the scarcity of high temporal resolution marine records. Here, we present a reconstruction of Sea Surface Temperatures (SSTs) over the past twomillennia at unprecedented temporal resolution (2...

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Published in:Earth and Planetary Science Letters
Main Authors: Sicre, Marie Alexandrine, Jacob, Jérémy, Ezat, Ullah, Rousse, Sonia, Kissel, Catherine, Yiou, Pascal, Eiríksson, Jon, Knudsen, Karen Luise, Jansen, Eystein, Turon, Jean-Louis
Other Authors: Paléocéanographie (PALEOCEAN), Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Institut des Sciences de la Terre d'Orléans (ISTO), Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS), Climat et Magnétisme (CLIMAG), Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR), University of Iceland Reykjavik, Department of Earth Sciences Aarhus, Aarhus University Aarhus, Bjerknes Centre for Climate Research (BCCR), Department of Biological Sciences Bergen (BIO / UiB), University of Bergen (UiB)-University of Bergen (UiB), Departement de Géologie et Océanographie, Université Sciences et Technologies - Bordeaux 1 (UB), PACLIVA European Commission 5th Framework Program (Contract EVK2-2002-00143).
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2008
Subjects:
Online Access:https://insu.hal.science/insu-00311666
https://insu.hal.science/insu-00311666/document
https://insu.hal.science/insu-00311666/file/Sicre_et_al_-_2008_-_EPSL.pdf
https://doi.org/10.1016/j.epsl.2008.01.011
id ftceafr:oai:HAL:insu-00311666v1
record_format openpolar
institution Open Polar
collection HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives)
op_collection_id ftceafr
language English
topic Decadal variability
Sea surface temperature
North Atlantic
Alkenones
Medieval Warm Period
Little Ice Age
Iceland
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
spellingShingle Decadal variability
Sea surface temperature
North Atlantic
Alkenones
Medieval Warm Period
Little Ice Age
Iceland
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
Sicre, Marie Alexandrine
Jacob, Jérémy
Ezat, Ullah
Rousse, Sonia
Kissel, Catherine
Yiou, Pascal
Eiríksson, Jon
Knudsen, Karen Luise
Jansen, Eystein
Turon, Jean-Louis
Decadal variability of sea surface temperatures off North Iceland over the last 2000 years
topic_facet Decadal variability
Sea surface temperature
North Atlantic
Alkenones
Medieval Warm Period
Little Ice Age
Iceland
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
description International audience Ocean variability at decadal time-scales remains poorly described partly because of the scarcity of high temporal resolution marine records. Here, we present a reconstruction of Sea Surface Temperatures (SSTs) over the past twomillennia at unprecedented temporal resolution (2 to 5 years), from a marine core located off North Iceland. Alkenone paleothermometry was used to infer SST variability, and tephrochronology to build the age model. Spectral analyses of the SSTsignal indicate intermittent 20–25 year oscillations, with periods of strong and weak power, that are likely reflecting the ocean response to wind forcing, presumably the North Atlantic Oscillation (NAO). Warmer SSTs and paleo-magnetic proxy data, between 1000 and 1350 year A.D., overlapping theMedievalWarm Period (MWP), suggest enhanced heat transport across the Denmark Strait by the North Icelandic IrmingerCurrent (NIIC). This is in contrast with the subsequent period, which includes the Little IceAge (LIA), showing continuous cooling towards the 20th century.Reduced NIIC flow through theDenmark Strait likely resulting from higher freshwater and sea ice export from the Arctic would account for the observed colder conditions.
author2 Paléocéanographie (PALEOCEAN)
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
Institut des Sciences de la Terre d'Orléans (ISTO)
Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)
Climat et Magnétisme (CLIMAG)
Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR)
University of Iceland Reykjavik
Department of Earth Sciences Aarhus
Aarhus University Aarhus
Bjerknes Centre for Climate Research (BCCR)
Department of Biological Sciences Bergen (BIO / UiB)
University of Bergen (UiB)-University of Bergen (UiB)
Departement de Géologie et Océanographie
Université Sciences et Technologies - Bordeaux 1 (UB)
PACLIVA European Commission 5th Framework Program (Contract EVK2-2002-00143).
format Article in Journal/Newspaper
author Sicre, Marie Alexandrine
Jacob, Jérémy
Ezat, Ullah
Rousse, Sonia
Kissel, Catherine
Yiou, Pascal
Eiríksson, Jon
Knudsen, Karen Luise
Jansen, Eystein
Turon, Jean-Louis
author_facet Sicre, Marie Alexandrine
Jacob, Jérémy
Ezat, Ullah
Rousse, Sonia
Kissel, Catherine
Yiou, Pascal
Eiríksson, Jon
Knudsen, Karen Luise
Jansen, Eystein
Turon, Jean-Louis
author_sort Sicre, Marie Alexandrine
title Decadal variability of sea surface temperatures off North Iceland over the last 2000 years
title_short Decadal variability of sea surface temperatures off North Iceland over the last 2000 years
title_full Decadal variability of sea surface temperatures off North Iceland over the last 2000 years
title_fullStr Decadal variability of sea surface temperatures off North Iceland over the last 2000 years
title_full_unstemmed Decadal variability of sea surface temperatures off North Iceland over the last 2000 years
title_sort decadal variability of sea surface temperatures off north iceland over the last 2000 years
publisher HAL CCSD
publishDate 2008
url https://insu.hal.science/insu-00311666
https://insu.hal.science/insu-00311666/document
https://insu.hal.science/insu-00311666/file/Sicre_et_al_-_2008_-_EPSL.pdf
https://doi.org/10.1016/j.epsl.2008.01.011
genre Denmark Strait
Iceland
North Atlantic
North Atlantic oscillation
Sea ice
NIIC
genre_facet Denmark Strait
Iceland
North Atlantic
North Atlantic oscillation
Sea ice
NIIC
op_source ISSN: 0012-821X
Earth and Planetary Science Letters
https://insu.hal.science/insu-00311666
Earth and Planetary Science Letters, 2008, 268, pp.137-142. ⟨10.1016/j.epsl.2008.01.011⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.epsl.2008.01.011
insu-00311666
https://insu.hal.science/insu-00311666
https://insu.hal.science/insu-00311666/document
https://insu.hal.science/insu-00311666/file/Sicre_et_al_-_2008_-_EPSL.pdf
doi:10.1016/j.epsl.2008.01.011
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1016/j.epsl.2008.01.011
container_title Earth and Planetary Science Letters
container_volume 268
container_issue 1-2
container_start_page 137
op_container_end_page 142
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spelling ftceafr:oai:HAL:insu-00311666v1 2024-09-15T18:03:37+00:00 Decadal variability of sea surface temperatures off North Iceland over the last 2000 years Sicre, Marie Alexandrine Jacob, Jérémy Ezat, Ullah Rousse, Sonia Kissel, Catherine Yiou, Pascal Eiríksson, Jon Knudsen, Karen Luise Jansen, Eystein Turon, Jean-Louis Paléocéanographie (PALEOCEAN) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Institut des Sciences de la Terre d'Orléans (ISTO) Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS) Climat et Magnétisme (CLIMAG) Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR) University of Iceland Reykjavik Department of Earth Sciences Aarhus Aarhus University Aarhus Bjerknes Centre for Climate Research (BCCR) Department of Biological Sciences Bergen (BIO / UiB) University of Bergen (UiB)-University of Bergen (UiB) Departement de Géologie et Océanographie Université Sciences et Technologies - Bordeaux 1 (UB) PACLIVA European Commission 5th Framework Program (Contract EVK2-2002-00143). 2008 https://insu.hal.science/insu-00311666 https://insu.hal.science/insu-00311666/document https://insu.hal.science/insu-00311666/file/Sicre_et_al_-_2008_-_EPSL.pdf https://doi.org/10.1016/j.epsl.2008.01.011 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.epsl.2008.01.011 insu-00311666 https://insu.hal.science/insu-00311666 https://insu.hal.science/insu-00311666/document https://insu.hal.science/insu-00311666/file/Sicre_et_al_-_2008_-_EPSL.pdf doi:10.1016/j.epsl.2008.01.011 info:eu-repo/semantics/OpenAccess ISSN: 0012-821X Earth and Planetary Science Letters https://insu.hal.science/insu-00311666 Earth and Planetary Science Letters, 2008, 268, pp.137-142. ⟨10.1016/j.epsl.2008.01.011⟩ Decadal variability Sea surface temperature North Atlantic Alkenones Medieval Warm Period Little Ice Age Iceland [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2008 ftceafr https://doi.org/10.1016/j.epsl.2008.01.011 2024-07-22T13:16:34Z International audience Ocean variability at decadal time-scales remains poorly described partly because of the scarcity of high temporal resolution marine records. Here, we present a reconstruction of Sea Surface Temperatures (SSTs) over the past twomillennia at unprecedented temporal resolution (2 to 5 years), from a marine core located off North Iceland. Alkenone paleothermometry was used to infer SST variability, and tephrochronology to build the age model. Spectral analyses of the SSTsignal indicate intermittent 20–25 year oscillations, with periods of strong and weak power, that are likely reflecting the ocean response to wind forcing, presumably the North Atlantic Oscillation (NAO). Warmer SSTs and paleo-magnetic proxy data, between 1000 and 1350 year A.D., overlapping theMedievalWarm Period (MWP), suggest enhanced heat transport across the Denmark Strait by the North Icelandic IrmingerCurrent (NIIC). This is in contrast with the subsequent period, which includes the Little IceAge (LIA), showing continuous cooling towards the 20th century.Reduced NIIC flow through theDenmark Strait likely resulting from higher freshwater and sea ice export from the Arctic would account for the observed colder conditions. Article in Journal/Newspaper Denmark Strait Iceland North Atlantic North Atlantic oscillation Sea ice NIIC HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) Earth and Planetary Science Letters 268 1-2 137 142