The Arctic Winter Sea Ice Quadrupole Revisited
International audience The dominant mode of Arctic sea ice variability in winter is often maintained to be represented by a quadrupole structure, comprising poles of one sign in the Okhotsk, Greenland and Barents Seas, and opposing sign in the Labrador and Bering Seas, forced by the North Atlantic O...
Published in: | Journal of Climate |
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Main Authors: | , , |
Other Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2017
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Online Access: | https://hal.sorbonne-universite.fr/hal-01452684 https://hal.sorbonne-universite.fr/hal-01452684v2/document https://hal.sorbonne-universite.fr/hal-01452684v2/file/jcli-d-16-0506.1.pdf https://doi.org/10.1175/JCLI-D-16-0506.1 |
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Open Polar |
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Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
Interdecadal variability Interannual variability Sea ice Arctic [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
spellingShingle |
Interdecadal variability Interannual variability Sea ice Arctic [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology Close, Sally Houssais, Marie-Noëlle Herbaut, Christophe The Arctic Winter Sea Ice Quadrupole Revisited |
topic_facet |
Interdecadal variability Interannual variability Sea ice Arctic [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
description |
International audience The dominant mode of Arctic sea ice variability in winter is often maintained to be represented by a quadrupole structure, comprising poles of one sign in the Okhotsk, Greenland and Barents Seas, and opposing sign in the Labrador and Bering Seas, forced by the North Atlantic Oscillation. In this study, we revisit this large-scale winter mode of sea ice variability using microwave satellite and reanalysis data. We find that the quadrupole structure does not describe a significant covariance relationship amongst all four component poles. The first empirical orthogonal mode, explaining covariability in the sea ice of the Barents, Greenland and Okhotsk Seas, is linked to the Siberian High, whilst the North Atlantic Oscillation exhibits a significant relationship only with the Labrador Sea ice, which varies independently as the second mode. The principal components are characterised by a strong low-frequency signal; the satellite record still being short, statistical analyses should thus be applied cautiously. |
author2 |
Variabilité de l'Océan et de la Glace de mer (VOG) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) The research leading to these results has received funding from the European Union 7th Framework Programme (FP7 2007–13) under Grant Agreement 308299, NACLIM Project. European Project: 308299,EC:FP7:ENV,FP7-ENV-2012-two-stage,NACLIM(2012) |
format |
Article in Journal/Newspaper |
author |
Close, Sally Houssais, Marie-Noëlle Herbaut, Christophe |
author_facet |
Close, Sally Houssais, Marie-Noëlle Herbaut, Christophe |
author_sort |
Close, Sally |
title |
The Arctic Winter Sea Ice Quadrupole Revisited |
title_short |
The Arctic Winter Sea Ice Quadrupole Revisited |
title_full |
The Arctic Winter Sea Ice Quadrupole Revisited |
title_fullStr |
The Arctic Winter Sea Ice Quadrupole Revisited |
title_full_unstemmed |
The Arctic Winter Sea Ice Quadrupole Revisited |
title_sort |
arctic winter sea ice quadrupole revisited |
publisher |
HAL CCSD |
publishDate |
2017 |
url |
https://hal.sorbonne-universite.fr/hal-01452684 https://hal.sorbonne-universite.fr/hal-01452684v2/document https://hal.sorbonne-universite.fr/hal-01452684v2/file/jcli-d-16-0506.1.pdf https://doi.org/10.1175/JCLI-D-16-0506.1 |
genre |
Arctic Arctic Greenland Labrador Sea North Atlantic North Atlantic oscillation Sea ice |
genre_facet |
Arctic Arctic Greenland Labrador Sea North Atlantic North Atlantic oscillation Sea ice |
op_source |
ISSN: 0894-8755 EISSN: 1520-0442 Journal of Climate https://hal.sorbonne-universite.fr/hal-01452684 Journal of Climate, 2017, 30, pp.3157-3167. ⟨10.1175/JCLI-D-16-0506.1⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1175/JCLI-D-16-0506.1 info:eu-repo/grantAgreement/EC/FP7/308299/EU/North Atlantic Climate: Predictability of the climate in the North Atlantic/European sector related to North Atlantic/Arctic sea surface temperature and sea ice variability and change/NACLIM hal-01452684 https://hal.sorbonne-universite.fr/hal-01452684 https://hal.sorbonne-universite.fr/hal-01452684v2/document https://hal.sorbonne-universite.fr/hal-01452684v2/file/jcli-d-16-0506.1.pdf BIBCODE: 2017JCli.30.3157C doi:10.1175/JCLI-D-16-0506.1 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1175/JCLI-D-16-0506.1 |
container_title |
Journal of Climate |
container_volume |
30 |
container_issue |
9 |
container_start_page |
3157 |
op_container_end_page |
3167 |
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1797575312748314624 |
spelling |
ftinsu:oai:HAL:hal-01452684v2 2024-04-28T08:04:59+00:00 The Arctic Winter Sea Ice Quadrupole Revisited Close, Sally Houssais, Marie-Noëlle Herbaut, Christophe Variabilité de l'Océan et de la Glace de mer (VOG) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) The research leading to these results has received funding from the European Union 7th Framework Programme (FP7 2007–13) under Grant Agreement 308299, NACLIM Project. European Project: 308299,EC:FP7:ENV,FP7-ENV-2012-two-stage,NACLIM(2012) 2017 https://hal.sorbonne-universite.fr/hal-01452684 https://hal.sorbonne-universite.fr/hal-01452684v2/document https://hal.sorbonne-universite.fr/hal-01452684v2/file/jcli-d-16-0506.1.pdf https://doi.org/10.1175/JCLI-D-16-0506.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/JCLI-D-16-0506.1 info:eu-repo/grantAgreement/EC/FP7/308299/EU/North Atlantic Climate: Predictability of the climate in the North Atlantic/European sector related to North Atlantic/Arctic sea surface temperature and sea ice variability and change/NACLIM hal-01452684 https://hal.sorbonne-universite.fr/hal-01452684 https://hal.sorbonne-universite.fr/hal-01452684v2/document https://hal.sorbonne-universite.fr/hal-01452684v2/file/jcli-d-16-0506.1.pdf BIBCODE: 2017JCli.30.3157C doi:10.1175/JCLI-D-16-0506.1 info:eu-repo/semantics/OpenAccess ISSN: 0894-8755 EISSN: 1520-0442 Journal of Climate https://hal.sorbonne-universite.fr/hal-01452684 Journal of Climate, 2017, 30, pp.3157-3167. ⟨10.1175/JCLI-D-16-0506.1⟩ Interdecadal variability Interannual variability Sea ice Arctic [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2017 ftinsu https://doi.org/10.1175/JCLI-D-16-0506.1 2024-04-05T00:47:53Z International audience The dominant mode of Arctic sea ice variability in winter is often maintained to be represented by a quadrupole structure, comprising poles of one sign in the Okhotsk, Greenland and Barents Seas, and opposing sign in the Labrador and Bering Seas, forced by the North Atlantic Oscillation. In this study, we revisit this large-scale winter mode of sea ice variability using microwave satellite and reanalysis data. We find that the quadrupole structure does not describe a significant covariance relationship amongst all four component poles. The first empirical orthogonal mode, explaining covariability in the sea ice of the Barents, Greenland and Okhotsk Seas, is linked to the Siberian High, whilst the North Atlantic Oscillation exhibits a significant relationship only with the Labrador Sea ice, which varies independently as the second mode. The principal components are characterised by a strong low-frequency signal; the satellite record still being short, statistical analyses should thus be applied cautiously. Article in Journal/Newspaper Arctic Arctic Greenland Labrador Sea North Atlantic North Atlantic oscillation Sea ice Institut national des sciences de l'Univers: HAL-INSU Journal of Climate 30 9 3157 3167 |