On the spatial coherence of the Atlantic Water inflow across the Nordic Seas
International audience The co-variability of the Atlantic Water (AW) branches in the Nordic Seas is investigated over the period 1979-2012 using an eddy permitting model. A noticeable circulation change is found in the mid-1990s. Prior to the mid-1990s, the leading mode of variability defines a larg...
Published in: | Journal of Geophysical Research: Oceans |
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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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Subjects: | |
Online Access: | https://hal.sorbonne-universite.fr/hal-01514935 https://hal.sorbonne-universite.fr/hal-01514935/document https://hal.sorbonne-universite.fr/hal-01514935/file/Herbaut_et_al-2017-Journal_of_Geophysical_Research__Oceans.pdf https://doi.org/10.1002/2016JC012566 |
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Open Polar |
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Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
spellingShingle |
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography Herbaut, Christophe Houssais, Marie-Noëlle Close, Sally Blaizot, Anne-Cécile On the spatial coherence of the Atlantic Water inflow across the Nordic Seas |
topic_facet |
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
description |
International audience The co-variability of the Atlantic Water (AW) branches in the Nordic Seas is investigated over the period 1979-2012 using an eddy permitting model. A noticeable circulation change is found in the mid-1990s. Prior to the mid-1990s, the leading mode of variability defines a large scale pattern, with concomitant variations in the Atlantic Water (AW) inflow in the Faroe-Shetland Channel (FSC), the Norwegian Atlantic Slope Current (NwASC), the AW inflow to the Barents Sea and the West Spitsbergen Current (WSC). After the mid-1990s, the co-variability between the NwASC and the AW inflow in both the FSC and the WSC is lost. Consequently, the northern Barents Sea circulation anomaly pattern, which is present throughout the full period, becomes the leading mode of circulation in the northern Nordic Seas after the mid-1990s. The circulation change of the mid-1990s appears to be linked to a weakening of the southwesterly wind anomalies in Norwegian Sea, as the northern center of action of the first mode of sea level pressure (NAO) weakens. Passive tracer experiments suggest that this circulation change may be accompanied by increased heat transfer from the AW current to the interior Nordic Seas. This in turn may have limited the influence of the recently observed AW warming in the Iceland-Scotland Passage on the NwASC downstream. |
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) European Project: 308299,EC:FP7:ENV,FP7-ENV-2012-two-stage,NACLIM(2012) |
format |
Article in Journal/Newspaper |
author |
Herbaut, Christophe Houssais, Marie-Noëlle Close, Sally Blaizot, Anne-Cécile |
author_facet |
Herbaut, Christophe Houssais, Marie-Noëlle Close, Sally Blaizot, Anne-Cécile |
author_sort |
Herbaut, Christophe |
title |
On the spatial coherence of the Atlantic Water inflow across the Nordic Seas |
title_short |
On the spatial coherence of the Atlantic Water inflow across the Nordic Seas |
title_full |
On the spatial coherence of the Atlantic Water inflow across the Nordic Seas |
title_fullStr |
On the spatial coherence of the Atlantic Water inflow across the Nordic Seas |
title_full_unstemmed |
On the spatial coherence of the Atlantic Water inflow across the Nordic Seas |
title_sort |
on the spatial coherence of the atlantic water inflow across the nordic seas |
publisher |
HAL CCSD |
publishDate |
2017 |
url |
https://hal.sorbonne-universite.fr/hal-01514935 https://hal.sorbonne-universite.fr/hal-01514935/document https://hal.sorbonne-universite.fr/hal-01514935/file/Herbaut_et_al-2017-Journal_of_Geophysical_Research__Oceans.pdf https://doi.org/10.1002/2016JC012566 |
geographic |
Barents Sea Norwegian Sea |
geographic_facet |
Barents Sea Norwegian Sea |
genre |
Arctic Barents Sea Iceland Nordic Seas Norwegian Sea Spitsbergen |
genre_facet |
Arctic Barents Sea Iceland Nordic Seas Norwegian Sea Spitsbergen |
op_source |
ISSN: 2169-9275 EISSN: 2169-9291 Journal of Geophysical Research. Oceans https://hal.sorbonne-universite.fr/hal-01514935 Journal of Geophysical Research. Oceans, 2017, 122 (5), pp.4346-4363. ⟨10.1002/2016JC012566⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1002/2016JC012566 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-01514935 https://hal.sorbonne-universite.fr/hal-01514935 https://hal.sorbonne-universite.fr/hal-01514935/document https://hal.sorbonne-universite.fr/hal-01514935/file/Herbaut_et_al-2017-Journal_of_Geophysical_Research__Oceans.pdf BIBCODE: 2017JGRC.122.4346H doi:10.1002/2016JC012566 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1002/2016JC012566 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
122 |
container_issue |
5 |
container_start_page |
4346 |
op_container_end_page |
4363 |
_version_ |
1766301866935713792 |
spelling |
ftunivnantes:oai:HAL:hal-01514935v1 2023-05-15T14:27:50+02:00 On the spatial coherence of the Atlantic Water inflow across the Nordic Seas Herbaut, Christophe Houssais, Marie-Noëlle Close, Sally Blaizot, Anne-Cécile 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) European Project: 308299,EC:FP7:ENV,FP7-ENV-2012-two-stage,NACLIM(2012) 2017 https://hal.sorbonne-universite.fr/hal-01514935 https://hal.sorbonne-universite.fr/hal-01514935/document https://hal.sorbonne-universite.fr/hal-01514935/file/Herbaut_et_al-2017-Journal_of_Geophysical_Research__Oceans.pdf https://doi.org/10.1002/2016JC012566 en eng HAL CCSD Wiley-Blackwell info:eu-repo/semantics/altIdentifier/doi/10.1002/2016JC012566 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-01514935 https://hal.sorbonne-universite.fr/hal-01514935 https://hal.sorbonne-universite.fr/hal-01514935/document https://hal.sorbonne-universite.fr/hal-01514935/file/Herbaut_et_al-2017-Journal_of_Geophysical_Research__Oceans.pdf BIBCODE: 2017JGRC.122.4346H doi:10.1002/2016JC012566 info:eu-repo/semantics/OpenAccess ISSN: 2169-9275 EISSN: 2169-9291 Journal of Geophysical Research. Oceans https://hal.sorbonne-universite.fr/hal-01514935 Journal of Geophysical Research. Oceans, 2017, 122 (5), pp.4346-4363. ⟨10.1002/2016JC012566⟩ [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography info:eu-repo/semantics/article Journal articles 2017 ftunivnantes https://doi.org/10.1002/2016JC012566 2023-01-18T01:10:56Z International audience The co-variability of the Atlantic Water (AW) branches in the Nordic Seas is investigated over the period 1979-2012 using an eddy permitting model. A noticeable circulation change is found in the mid-1990s. Prior to the mid-1990s, the leading mode of variability defines a large scale pattern, with concomitant variations in the Atlantic Water (AW) inflow in the Faroe-Shetland Channel (FSC), the Norwegian Atlantic Slope Current (NwASC), the AW inflow to the Barents Sea and the West Spitsbergen Current (WSC). After the mid-1990s, the co-variability between the NwASC and the AW inflow in both the FSC and the WSC is lost. Consequently, the northern Barents Sea circulation anomaly pattern, which is present throughout the full period, becomes the leading mode of circulation in the northern Nordic Seas after the mid-1990s. The circulation change of the mid-1990s appears to be linked to a weakening of the southwesterly wind anomalies in Norwegian Sea, as the northern center of action of the first mode of sea level pressure (NAO) weakens. Passive tracer experiments suggest that this circulation change may be accompanied by increased heat transfer from the AW current to the interior Nordic Seas. This in turn may have limited the influence of the recently observed AW warming in the Iceland-Scotland Passage on the NwASC downstream. Article in Journal/Newspaper Arctic Barents Sea Iceland Nordic Seas Norwegian Sea Spitsbergen Université de Nantes: HAL-UNIV-NANTES Barents Sea Norwegian Sea Journal of Geophysical Research: Oceans 122 5 4346 4363 |