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...
Published in: | Journal of Geophysical Research: Oceans |
---|---|
Main Authors: | , , , |
Other Authors: | , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
CCSD
2017
|
Subjects: | |
Online Access: | https://hal.science/hal-01630799 https://hal.science/hal-01630799v1/document https://hal.science/hal-01630799v1/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 |
_version_ | 1825509214238277632 |
---|---|
author | Rossby, T. Reverdin, Gilles Chafik, Léon Søiland, Henrik |
author2 | Graduate School of Oceanography Narragansett University of Rhode Island (URI) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Institut Pierre-Simon-Laplace (IPSL) 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)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-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)-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) |
author_facet | Rossby, T. Reverdin, Gilles Chafik, Léon Søiland, Henrik |
author_sort | Rossby, T. |
collection | Muséum National d'Histoire Naturelle (MNHM): HAL |
container_issue | 7 |
container_start_page | 5870 |
container_title | Journal of Geophysical Research: Oceans |
container_volume | 122 |
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. |
format | Article in Journal/Newspaper |
genre | Greenland North Atlantic |
genre_facet | Greenland North Atlantic |
geographic | Greenland Irminger Sea Rockall Trough |
geographic_facet | Greenland Irminger Sea Rockall Trough |
id | ftmuseumnhn:oai:HAL:hal-01630799v1 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-34.041,-34.041,63.054,63.054) ENVELOPE(-15.036,-15.036,53.825,53.825) |
op_collection_id | ftmuseumnhn |
op_container_end_page | 5887 |
op_doi | https://doi.org/10.1002/2017JC012835 |
op_relation | info:eu-repo/semantics/altIdentifier/doi/10.1002/2017JC012835 doi:10.1002/2017JC012835 WOS: 000409893600037 |
op_rights | http://hal.archives-ouvertes.fr/licences/copyright/ info:eu-repo/semantics/OpenAccess |
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⟩ |
publishDate | 2017 |
publisher | CCSD |
record_format | openpolar |
spelling | ftmuseumnhn:oai:HAL:hal-01630799v1 2025-03-02T15:29:14+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) Institut Pierre-Simon-Laplace (IPSL) 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)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-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)-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-01630799v1/document https://hal.science/hal-01630799v1/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 CCSD Wiley-Blackwell info:eu-repo/semantics/altIdentifier/doi/10.1002/2017JC012835 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 ftmuseumnhn https://doi.org/10.1002/2017JC012835 2025-02-20T15:30:04Z 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 Muséum National d'Histoire Naturelle (MNHM): HAL Greenland Irminger Sea ENVELOPE(-34.041,-34.041,63.054,63.054) Rockall Trough ENVELOPE(-15.036,-15.036,53.825,53.825) Journal of Geophysical Research: Oceans 122 7 5870 5887 |
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 |
title | 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_short | 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 |
topic | currents MOC heat flux freshwater flux [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] |
topic_facet | currents MOC heat flux freshwater flux [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] |
url | https://hal.science/hal-01630799 https://hal.science/hal-01630799v1/document https://hal.science/hal-01630799v1/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 |