The Atlantic Meridional Overturning Circulation in High-Resolution Models
International audience The Atlantic meridional overturning circulation (AMOC) represents the zonally integrated stream function of meridional volume transport in the Atlantic Basin. The AMOC plays an important role in transporting heat meridionally in the climate system. Observations suggest a heat...
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
2020
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Online Access: | https://hal.science/hal-02879812 https://hal.science/hal-02879812/document https://hal.science/hal-02879812/file/Hirschi2020.pdf https://doi.org/10.1029/2019JC015522 |
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Open Polar |
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Institut national des sciences de l'Univers: HAL-INSU |
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English |
topic |
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
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[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography Hirschi, Joël J. -M Barnier, Bernard Böning, Claus Biastoch, Arne Blaker, Adam, T Coward, Andrew Danilov, Sergey Drijfhout, Sybren Getzlaff, Klaus Griffies, Stephen, M Hasumi, Hiroyasu Hewitt, Helene Iovino, Doroteaciro Kawasaki, Takao Kiss, Andrew Koldunov, Nikolay Marzocchi, Alice Mecking, Jennifer, V Moat, Ben Molines, Jean-Marc Myers, Paul, G Penduff, Thierry Roberts, Malcolm Tréguier, Anne-Marie Sein, Dmitry, V Sidorenko, Dmitry Small, Justin Spence, Paul Thompson, Luanne Weijer, Wilbert Xu, Xiaobiao The Atlantic Meridional Overturning Circulation in High-Resolution Models |
topic_facet |
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
description |
International audience The Atlantic meridional overturning circulation (AMOC) represents the zonally integrated stream function of meridional volume transport in the Atlantic Basin. The AMOC plays an important role in transporting heat meridionally in the climate system. Observations suggest a heat transport by the AMOC of 1.3 PW at 26°N-a latitude which is close to where the Atlantic northward heat transport is thought to reach its maximum. This shapes the climate of the North Atlantic region as we know it today. In recent years there has been significant progress both in our ability to observe the AMOC in nature and to simulate it in numerical models. Most previous modeling investigations of the AMOC and its impact on climate have relied on models with horizontal resolution that does not resolve ocean mesoscale eddies and the dynamics of the Gulf Stream/North Atlantic Current system. As a result of recent increases in computing power, models are now being run that are able to represent mesoscale ocean dynamics and the circulation features that rely on them. The aim of this review is to describe new insights into the AMOC provided by high-resolution models. Furthermore, we will describe how high-resolution model simulations can help resolve outstanding challenges in our understanding of the AMOC. |
author2 |
Laboratoire des Écoulements Géophysiques et Industriels Grenoble (LEGI) Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) Leibniz-Institut für Meereswissenschaften (IFM-GEOMAR) National Oceanography Centre (NOC) Ocean and Earth Science Southampton University of Southampton-National Oceanography Centre (NOC) NOAA Geophysical Fluid Dynamics Laboratory (GFDL) National Oceanic and Atmospheric Administration (NOAA) Atmosphere and Ocean Research Institute Kashiwa-shi (AORI) The University of Tokyo (UTokyo) Euro-Mediterranean Center on Climate Change (CMCC) Institute of Hydraulic Engineering and Water Resources Management Vienna University of Technology (TU Wien) Laboratoire de physique des océans (LPO) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) |
format |
Article in Journal/Newspaper |
author |
Hirschi, Joël J. -M Barnier, Bernard Böning, Claus Biastoch, Arne Blaker, Adam, T Coward, Andrew Danilov, Sergey Drijfhout, Sybren Getzlaff, Klaus Griffies, Stephen, M Hasumi, Hiroyasu Hewitt, Helene Iovino, Doroteaciro Kawasaki, Takao Kiss, Andrew Koldunov, Nikolay Marzocchi, Alice Mecking, Jennifer, V Moat, Ben Molines, Jean-Marc Myers, Paul, G Penduff, Thierry Roberts, Malcolm Tréguier, Anne-Marie Sein, Dmitry, V Sidorenko, Dmitry Small, Justin Spence, Paul Thompson, Luanne Weijer, Wilbert Xu, Xiaobiao |
author_facet |
Hirschi, Joël J. -M Barnier, Bernard Böning, Claus Biastoch, Arne Blaker, Adam, T Coward, Andrew Danilov, Sergey Drijfhout, Sybren Getzlaff, Klaus Griffies, Stephen, M Hasumi, Hiroyasu Hewitt, Helene Iovino, Doroteaciro Kawasaki, Takao Kiss, Andrew Koldunov, Nikolay Marzocchi, Alice Mecking, Jennifer, V Moat, Ben Molines, Jean-Marc Myers, Paul, G Penduff, Thierry Roberts, Malcolm Tréguier, Anne-Marie Sein, Dmitry, V Sidorenko, Dmitry Small, Justin Spence, Paul Thompson, Luanne Weijer, Wilbert Xu, Xiaobiao |
author_sort |
Hirschi, Joël J. -M |
title |
The Atlantic Meridional Overturning Circulation in High-Resolution Models |
title_short |
The Atlantic Meridional Overturning Circulation in High-Resolution Models |
title_full |
The Atlantic Meridional Overturning Circulation in High-Resolution Models |
title_fullStr |
The Atlantic Meridional Overturning Circulation in High-Resolution Models |
title_full_unstemmed |
The Atlantic Meridional Overturning Circulation in High-Resolution Models |
title_sort |
atlantic meridional overturning circulation in high-resolution models |
publisher |
HAL CCSD |
publishDate |
2020 |
url |
https://hal.science/hal-02879812 https://hal.science/hal-02879812/document https://hal.science/hal-02879812/file/Hirschi2020.pdf https://doi.org/10.1029/2019JC015522 |
genre |
north atlantic current North Atlantic |
genre_facet |
north atlantic current North Atlantic |
op_source |
ISSN: 2169-9275 EISSN: 2169-9291 Journal of Geophysical Research. Oceans https://hal.science/hal-02879812 Journal of Geophysical Research. Oceans, 2020, ⟨10.1029/2019JC015522⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2019JC015522 hal-02879812 https://hal.science/hal-02879812 https://hal.science/hal-02879812/document https://hal.science/hal-02879812/file/Hirschi2020.pdf doi:10.1029/2019JC015522 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2019JC015522 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
125 |
container_issue |
4 |
_version_ |
1785569303822598144 |
spelling |
ftinsu:oai:HAL:hal-02879812v1 2023-12-17T10:45:59+01:00 The Atlantic Meridional Overturning Circulation in High-Resolution Models Hirschi, Joël J. -M Barnier, Bernard Böning, Claus Biastoch, Arne Blaker, Adam, T Coward, Andrew Danilov, Sergey Drijfhout, Sybren Getzlaff, Klaus Griffies, Stephen, M Hasumi, Hiroyasu Hewitt, Helene Iovino, Doroteaciro Kawasaki, Takao Kiss, Andrew Koldunov, Nikolay Marzocchi, Alice Mecking, Jennifer, V Moat, Ben Molines, Jean-Marc Myers, Paul, G Penduff, Thierry Roberts, Malcolm Tréguier, Anne-Marie Sein, Dmitry, V Sidorenko, Dmitry Small, Justin Spence, Paul Thompson, Luanne Weijer, Wilbert Xu, Xiaobiao Laboratoire des Écoulements Géophysiques et Industriels Grenoble (LEGI) Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) Leibniz-Institut für Meereswissenschaften (IFM-GEOMAR) National Oceanography Centre (NOC) Ocean and Earth Science Southampton University of Southampton-National Oceanography Centre (NOC) NOAA Geophysical Fluid Dynamics Laboratory (GFDL) National Oceanic and Atmospheric Administration (NOAA) Atmosphere and Ocean Research Institute Kashiwa-shi (AORI) The University of Tokyo (UTokyo) Euro-Mediterranean Center on Climate Change (CMCC) Institute of Hydraulic Engineering and Water Resources Management Vienna University of Technology (TU Wien) Laboratoire de physique des océans (LPO) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) 2020 https://hal.science/hal-02879812 https://hal.science/hal-02879812/document https://hal.science/hal-02879812/file/Hirschi2020.pdf https://doi.org/10.1029/2019JC015522 en eng HAL CCSD Wiley-Blackwell info:eu-repo/semantics/altIdentifier/doi/10.1029/2019JC015522 hal-02879812 https://hal.science/hal-02879812 https://hal.science/hal-02879812/document https://hal.science/hal-02879812/file/Hirschi2020.pdf doi:10.1029/2019JC015522 info:eu-repo/semantics/OpenAccess ISSN: 2169-9275 EISSN: 2169-9291 Journal of Geophysical Research. Oceans https://hal.science/hal-02879812 Journal of Geophysical Research. Oceans, 2020, ⟨10.1029/2019JC015522⟩ [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography info:eu-repo/semantics/article Journal articles 2020 ftinsu https://doi.org/10.1029/2019JC015522 2023-11-22T17:40:38Z International audience The Atlantic meridional overturning circulation (AMOC) represents the zonally integrated stream function of meridional volume transport in the Atlantic Basin. The AMOC plays an important role in transporting heat meridionally in the climate system. Observations suggest a heat transport by the AMOC of 1.3 PW at 26°N-a latitude which is close to where the Atlantic northward heat transport is thought to reach its maximum. This shapes the climate of the North Atlantic region as we know it today. In recent years there has been significant progress both in our ability to observe the AMOC in nature and to simulate it in numerical models. Most previous modeling investigations of the AMOC and its impact on climate have relied on models with horizontal resolution that does not resolve ocean mesoscale eddies and the dynamics of the Gulf Stream/North Atlantic Current system. As a result of recent increases in computing power, models are now being run that are able to represent mesoscale ocean dynamics and the circulation features that rely on them. The aim of this review is to describe new insights into the AMOC provided by high-resolution models. Furthermore, we will describe how high-resolution model simulations can help resolve outstanding challenges in our understanding of the AMOC. Article in Journal/Newspaper north atlantic current North Atlantic Institut national des sciences de l'Univers: HAL-INSU Journal of Geophysical Research: Oceans 125 4 |