A global probabilistic study of the ocean heat content low-frequency variability: Atmospheric forcing versus oceanic chaos

International audience A global 1/4 ∘ ocean/sea ice 50-member ensemble simulation is used to disentangle the low-frequency imprints of the atmospherically forced oceanic variability and of the chaotic intrinsic oceanic variability (IOV) on the large-scale (10 ∘ × 10 ∘) ocean heat content (OHC) betwe...

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Published in:Geophysical Research Letters
Main Authors: Sérazin, Guillaume, Jaymond, Alexandre, Leroux, Stephanie, Penduff, Thierry, Bessières, Laurent, Llovel, W., Barnier, Bernard, Molines, Jean-Marc, Terray, Laurent
Other Authors: Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ), Institut de Mathématiques de Bordeaux (IMB), Université Bordeaux Segalen - Bordeaux 2-Université Sciences et Technologies - Bordeaux 1 (UB)-Université de Bordeaux (UB)-Institut Polytechnique de Bordeaux (Bordeaux INP)-Centre National de la Recherche Scientifique (CNRS), Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), P.P. Shirshov Institute of Oceanology (SIO), Russian Academy of Sciences Moscow (RAS), Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique (CERFACS), Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique - CERFACS (CERFACS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2017
Subjects:
Online Access:https://hal.science/hal-03003527
https://hal.science/hal-03003527v2/document
https://hal.science/hal-03003527v2/file/2017GL073026.pdf
https://doi.org/10.1002/2017GL073026
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record_format openpolar
institution Open Polar
collection Université de Nantes: HAL-UNIV-NANTES
op_collection_id ftunivnantes
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
Sérazin, Guillaume
Jaymond, Alexandre
Leroux, Stephanie
Penduff, Thierry
Bessières, Laurent
Llovel, W.
Barnier, Bernard
Molines, Jean-Marc
Terray, Laurent
A global probabilistic study of the ocean heat content low-frequency variability: Atmospheric forcing versus oceanic chaos
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
description International audience A global 1/4 ∘ ocean/sea ice 50-member ensemble simulation is used to disentangle the low-frequency imprints of the atmospherically forced oceanic variability and of the chaotic intrinsic oceanic variability (IOV) on the large-scale (10 ∘ × 10 ∘) ocean heat content (OHC) between 1980 and 2010. The IOV explains most of the interannual-to-decadal large-scale OHC variance over substantial fractions of the global ocean area that increase with depth: 9%, 22%, and 31% in the 0-700 m, 700-2000 m and 2000 m bottom layers, respectively. Such areas concern principally eddy-active regions, mostly found in the Southern Ocean and in western boundary current extensions, and also concern the subtropical gyres at intermediate and deep levels. The oceanic chaos may also induce random multidecadal fluctuations so that large-scale regional OHC trends computed on the 1980-2010 period cannot be unambiguously attributed to the atmospheric forcing in several oceanic basins at various depths. These results are likely to raise detection and attribution issues from real observations.
author2 Institut des Géosciences de l’Environnement (IGE)
Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 )
Institut de Mathématiques de Bordeaux (IMB)
Université Bordeaux Segalen - Bordeaux 2-Université Sciences et Technologies - Bordeaux 1 (UB)-Université de Bordeaux (UB)-Institut Polytechnique de Bordeaux (Bordeaux INP)-Centre National de la Recherche Scientifique (CNRS)
Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)
P.P. Shirshov Institute of Oceanology (SIO)
Russian Academy of Sciences Moscow (RAS)
Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique (CERFACS)
Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique - CERFACS (CERFACS)
format Article in Journal/Newspaper
author Sérazin, Guillaume
Jaymond, Alexandre
Leroux, Stephanie
Penduff, Thierry
Bessières, Laurent
Llovel, W.
Barnier, Bernard
Molines, Jean-Marc
Terray, Laurent
author_facet Sérazin, Guillaume
Jaymond, Alexandre
Leroux, Stephanie
Penduff, Thierry
Bessières, Laurent
Llovel, W.
Barnier, Bernard
Molines, Jean-Marc
Terray, Laurent
author_sort Sérazin, Guillaume
title A global probabilistic study of the ocean heat content low-frequency variability: Atmospheric forcing versus oceanic chaos
title_short A global probabilistic study of the ocean heat content low-frequency variability: Atmospheric forcing versus oceanic chaos
title_full A global probabilistic study of the ocean heat content low-frequency variability: Atmospheric forcing versus oceanic chaos
title_fullStr A global probabilistic study of the ocean heat content low-frequency variability: Atmospheric forcing versus oceanic chaos
title_full_unstemmed A global probabilistic study of the ocean heat content low-frequency variability: Atmospheric forcing versus oceanic chaos
title_sort global probabilistic study of the ocean heat content low-frequency variability: atmospheric forcing versus oceanic chaos
publisher HAL CCSD
publishDate 2017
url https://hal.science/hal-03003527
https://hal.science/hal-03003527v2/document
https://hal.science/hal-03003527v2/file/2017GL073026.pdf
https://doi.org/10.1002/2017GL073026
geographic Southern Ocean
geographic_facet Southern Ocean
genre Sea ice
Southern Ocean
genre_facet Sea ice
Southern Ocean
op_source ISSN: 0094-8276
EISSN: 1944-8007
Geophysical Research Letters
https://hal.science/hal-03003527
Geophysical Research Letters, 2017, 44 (11), pp.5580-5589. ⟨10.1002/2017GL073026⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1002/2017GL073026
hal-03003527
https://hal.science/hal-03003527
https://hal.science/hal-03003527v2/document
https://hal.science/hal-03003527v2/file/2017GL073026.pdf
doi:10.1002/2017GL073026
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1002/2017GL073026
container_title Geophysical Research Letters
container_volume 44
container_issue 11
container_start_page 5580
op_container_end_page 5589
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spelling ftunivnantes:oai:HAL:hal-03003527v2 2023-05-15T18:18:22+02:00 A global probabilistic study of the ocean heat content low-frequency variability: Atmospheric forcing versus oceanic chaos Sérazin, Guillaume Jaymond, Alexandre Leroux, Stephanie Penduff, Thierry Bessières, Laurent Llovel, W. Barnier, Bernard Molines, Jean-Marc Terray, Laurent Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) Institut de Mathématiques de Bordeaux (IMB) Université Bordeaux Segalen - Bordeaux 2-Université Sciences et Technologies - Bordeaux 1 (UB)-Université de Bordeaux (UB)-Institut Polytechnique de Bordeaux (Bordeaux INP)-Centre National de la Recherche Scientifique (CNRS) Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS) P.P. Shirshov Institute of Oceanology (SIO) Russian Academy of Sciences Moscow (RAS) Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique (CERFACS) Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique - CERFACS (CERFACS) 2017-06-16 https://hal.science/hal-03003527 https://hal.science/hal-03003527v2/document https://hal.science/hal-03003527v2/file/2017GL073026.pdf https://doi.org/10.1002/2017GL073026 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1002/2017GL073026 hal-03003527 https://hal.science/hal-03003527 https://hal.science/hal-03003527v2/document https://hal.science/hal-03003527v2/file/2017GL073026.pdf doi:10.1002/2017GL073026 info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.science/hal-03003527 Geophysical Research Letters, 2017, 44 (11), pp.5580-5589. ⟨10.1002/2017GL073026⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2017 ftunivnantes https://doi.org/10.1002/2017GL073026 2023-03-01T02:34:59Z International audience A global 1/4 ∘ ocean/sea ice 50-member ensemble simulation is used to disentangle the low-frequency imprints of the atmospherically forced oceanic variability and of the chaotic intrinsic oceanic variability (IOV) on the large-scale (10 ∘ × 10 ∘) ocean heat content (OHC) between 1980 and 2010. The IOV explains most of the interannual-to-decadal large-scale OHC variance over substantial fractions of the global ocean area that increase with depth: 9%, 22%, and 31% in the 0-700 m, 700-2000 m and 2000 m bottom layers, respectively. Such areas concern principally eddy-active regions, mostly found in the Southern Ocean and in western boundary current extensions, and also concern the subtropical gyres at intermediate and deep levels. The oceanic chaos may also induce random multidecadal fluctuations so that large-scale regional OHC trends computed on the 1980-2010 period cannot be unambiguously attributed to the atmospheric forcing in several oceanic basins at various depths. These results are likely to raise detection and attribution issues from real observations. Article in Journal/Newspaper Sea ice Southern Ocean Université de Nantes: HAL-UNIV-NANTES Southern Ocean Geophysical Research Letters 44 11 5580 5589