A direct estimate of poleward volume, heat, and freshwater fluxes at 59.5°N between Greenland and Scotland

International audience The meridional overturning circulation (MOC) in the North Atlantic plays a major role in the transport of heat from low to high latitudes. In this study, we combine recent measurements of currents from the surface to >700 m from a shipboard acoustic Doppler current profiler...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Rossby, T., Reverdin, Gilles, Chafik, Léon, Søiland, Henrik
Other Authors: Graduate School of Oceanography Narragansett, University of Rhode Island (URI), 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), Bjerknes Centre for Climate Research (BCCR), Department of Biological Sciences Bergen (BIO / UiB), University of Bergen (UiB)-University of Bergen (UiB)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2017
Subjects:
MOC
Online Access:https://hal.science/hal-01630799
https://hal.science/hal-01630799/document
https://hal.science/hal-01630799/file/JGR%20Oceans%20-%202017%20-%20Rossby%20-%20A%20direct%20estimate%20of%20poleward%20volume%20heat%20and%20freshwater%20fluxes%20at%2059%205%20N%20between%20Greenland.pdf
https://doi.org/10.1002/2017JC012835
id ftsorbonneuniv:oai:HAL:hal-01630799v1
record_format openpolar
institution Open Polar
collection HAL Sorbonne Université
op_collection_id ftsorbonneuniv
language English
topic currents
MOC
heat flux
freshwater flux
[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
spellingShingle currents
MOC
heat flux
freshwater flux
[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
Rossby, T.
Reverdin, Gilles
Chafik, Léon
Søiland, Henrik
A direct estimate of poleward volume, heat, and freshwater fluxes at 59.5°N between Greenland and Scotland
topic_facet currents
MOC
heat flux
freshwater flux
[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
description International audience The meridional overturning circulation (MOC) in the North Atlantic plays a major role in the transport of heat from low to high latitudes. In this study, we combine recent measurements of currents from the surface to >700 m from a shipboard acoustic Doppler current profiler with Argo profiles (to 2000 m) to estimate poleward volume, heat, and freshwater flux at 59.5°N between Greenland and Scotland. This is made possible thanks to the vessel Nuka Arctica that operates on a 3 week schedule between Greenland and Denmark. For the period late 2012 to early 2016, the deseasoned mean meridional overturning circulation reaches a 18.4 ± 3.4 Sv maximum at the σθ = 27.55 kg m -3 isopycnal, which varies in depth from near the surface in the western Irminger Sea to 1000 m in Rockall Trough. The total heat and freshwater fluxes across 59.5°N = 399 ± 74 TW and −0.20 ± 0.04 Sv, where the uncertainties are principally due to that of the MOC. Analysis of altimetric sea surface height variations along exactly the same route reveals a somewhat stronger geostrophic flow north during this period compared to the 23 year mean suggesting that for a long-term mean the above flux estimates should be reduced slightly to 17.4 Sv, 377 TW, and −0.19 Sv, respectively, with the same estimate uncertainties. The ADCP program is ongoing.
author2 Graduate School of Oceanography Narragansett
University of Rhode Island (URI)
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)
Bjerknes Centre for Climate Research (BCCR)
Department of Biological Sciences Bergen (BIO / UiB)
University of Bergen (UiB)-University of Bergen (UiB)
format Article in Journal/Newspaper
author Rossby, T.
Reverdin, Gilles
Chafik, Léon
Søiland, Henrik
author_facet Rossby, T.
Reverdin, Gilles
Chafik, Léon
Søiland, Henrik
author_sort Rossby, T.
title A direct estimate of poleward volume, heat, and freshwater fluxes at 59.5°N between Greenland and Scotland
title_short A direct estimate of poleward volume, heat, and freshwater fluxes at 59.5°N between Greenland and Scotland
title_full A direct estimate of poleward volume, heat, and freshwater fluxes at 59.5°N between Greenland and Scotland
title_fullStr A direct estimate of poleward volume, heat, and freshwater fluxes at 59.5°N between Greenland and Scotland
title_full_unstemmed A direct estimate of poleward volume, heat, and freshwater fluxes at 59.5°N between Greenland and Scotland
title_sort direct estimate of poleward volume, heat, and freshwater fluxes at 59.5°n between greenland and scotland
publisher HAL CCSD
publishDate 2017
url https://hal.science/hal-01630799
https://hal.science/hal-01630799/document
https://hal.science/hal-01630799/file/JGR%20Oceans%20-%202017%20-%20Rossby%20-%20A%20direct%20estimate%20of%20poleward%20volume%20heat%20and%20freshwater%20fluxes%20at%2059%205%20N%20between%20Greenland.pdf
https://doi.org/10.1002/2017JC012835
genre Greenland
North Atlantic
genre_facet Greenland
North Atlantic
op_source ISSN: 2169-9275
EISSN: 2169-9291
Journal of Geophysical Research. Oceans
https://hal.science/hal-01630799
Journal of Geophysical Research. Oceans, 2017, 122 (7), pp.5870 - 5887. ⟨10.1002/2017JC012835⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1002/2017JC012835
hal-01630799
https://hal.science/hal-01630799
https://hal.science/hal-01630799/document
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doi:10.1002/2017JC012835
WOS: 000409893600037
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container_title Journal of Geophysical Research: Oceans
container_volume 122
container_issue 7
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spelling ftsorbonneuniv:oai:HAL:hal-01630799v1 2024-05-19T07:41:12+00:00 A direct estimate of poleward volume, heat, and freshwater fluxes at 59.5°N between Greenland and Scotland Rossby, T. Reverdin, Gilles Chafik, Léon Søiland, Henrik Graduate School of Oceanography Narragansett University of Rhode Island (URI) 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) Bjerknes Centre for Climate Research (BCCR) Department of Biological Sciences Bergen (BIO / UiB) University of Bergen (UiB)-University of Bergen (UiB) 2017-07 https://hal.science/hal-01630799 https://hal.science/hal-01630799/document https://hal.science/hal-01630799/file/JGR%20Oceans%20-%202017%20-%20Rossby%20-%20A%20direct%20estimate%20of%20poleward%20volume%20heat%20and%20freshwater%20fluxes%20at%2059%205%20N%20between%20Greenland.pdf https://doi.org/10.1002/2017JC012835 en eng HAL CCSD Wiley-Blackwell info:eu-repo/semantics/altIdentifier/doi/10.1002/2017JC012835 hal-01630799 https://hal.science/hal-01630799 https://hal.science/hal-01630799/document https://hal.science/hal-01630799/file/JGR%20Oceans%20-%202017%20-%20Rossby%20-%20A%20direct%20estimate%20of%20poleward%20volume%20heat%20and%20freshwater%20fluxes%20at%2059%205%20N%20between%20Greenland.pdf doi:10.1002/2017JC012835 WOS: 000409893600037 http://hal.archives-ouvertes.fr/licences/copyright/ info:eu-repo/semantics/OpenAccess ISSN: 2169-9275 EISSN: 2169-9291 Journal of Geophysical Research. Oceans https://hal.science/hal-01630799 Journal of Geophysical Research. Oceans, 2017, 122 (7), pp.5870 - 5887. ⟨10.1002/2017JC012835⟩ currents MOC heat flux freshwater flux [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] info:eu-repo/semantics/article Journal articles 2017 ftsorbonneuniv https://doi.org/10.1002/2017JC012835 2024-04-25T03:55:59Z International audience The meridional overturning circulation (MOC) in the North Atlantic plays a major role in the transport of heat from low to high latitudes. In this study, we combine recent measurements of currents from the surface to >700 m from a shipboard acoustic Doppler current profiler with Argo profiles (to 2000 m) to estimate poleward volume, heat, and freshwater flux at 59.5°N between Greenland and Scotland. This is made possible thanks to the vessel Nuka Arctica that operates on a 3 week schedule between Greenland and Denmark. For the period late 2012 to early 2016, the deseasoned mean meridional overturning circulation reaches a 18.4 ± 3.4 Sv maximum at the σθ = 27.55 kg m -3 isopycnal, which varies in depth from near the surface in the western Irminger Sea to 1000 m in Rockall Trough. The total heat and freshwater fluxes across 59.5°N = 399 ± 74 TW and −0.20 ± 0.04 Sv, where the uncertainties are principally due to that of the MOC. Analysis of altimetric sea surface height variations along exactly the same route reveals a somewhat stronger geostrophic flow north during this period compared to the 23 year mean suggesting that for a long-term mean the above flux estimates should be reduced slightly to 17.4 Sv, 377 TW, and −0.19 Sv, respectively, with the same estimate uncertainties. The ADCP program is ongoing. Article in Journal/Newspaper Greenland North Atlantic HAL Sorbonne Université Journal of Geophysical Research: Oceans 122 7 5870 5887