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) between...
Published in: | Geophysical Research Letters |
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Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
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Online Access: | https://hal.archives-ouvertes.fr/hal-01893878 https://hal.archives-ouvertes.fr/hal-01893878/document https://hal.archives-ouvertes.fr/hal-01893878/file/Serazin2017.pdf https://doi.org/10.1002/2017GL073026 |
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ftinsu:oai:HAL:hal-01893878v1 2023-05-15T18:18:29+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 ) Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique (CERFACS) CERFACS 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) 2017 https://hal.archives-ouvertes.fr/hal-01893878 https://hal.archives-ouvertes.fr/hal-01893878/document https://hal.archives-ouvertes.fr/hal-01893878/file/Serazin2017.pdf https://doi.org/10.1002/2017GL073026 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1002/2017GL073026 hal-01893878 https://hal.archives-ouvertes.fr/hal-01893878 https://hal.archives-ouvertes.fr/hal-01893878/document https://hal.archives-ouvertes.fr/hal-01893878/file/Serazin2017.pdf doi:10.1002/2017GL073026 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.archives-ouvertes.fr/hal-01893878 Geophysical Research Letters, American Geophysical Union, 2017, 44 (11), pp.5580-5589. ⟨10.1002/2017GL073026⟩ ocean heat content intrinsic variability eddy‐permitting OGCM climate change [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography info:eu-repo/semantics/article Journal articles 2017 ftinsu https://doi.org/10.1002/2017GL073026 2022-11-23T17:41:59Z 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 Institut national des sciences de l'Univers: HAL-INSU Southern Ocean Geophysical Research Letters 44 11 5580 5589 |
institution |
Open Polar |
collection |
Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
ocean heat content intrinsic variability eddy‐permitting OGCM climate change [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
spellingShingle |
ocean heat content intrinsic variability eddy‐permitting OGCM climate change [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography 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 |
ocean heat content intrinsic variability eddy‐permitting OGCM climate change [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
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 ) Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique (CERFACS) CERFACS 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) |
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.archives-ouvertes.fr/hal-01893878 https://hal.archives-ouvertes.fr/hal-01893878/document https://hal.archives-ouvertes.fr/hal-01893878/file/Serazin2017.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.archives-ouvertes.fr/hal-01893878 Geophysical Research Letters, American Geophysical Union, 2017, 44 (11), pp.5580-5589. ⟨10.1002/2017GL073026⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1002/2017GL073026 hal-01893878 https://hal.archives-ouvertes.fr/hal-01893878 https://hal.archives-ouvertes.fr/hal-01893878/document https://hal.archives-ouvertes.fr/hal-01893878/file/Serazin2017.pdf doi:10.1002/2017GL073026 |
op_rights |
http://creativecommons.org/licenses/by/ 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 |
_version_ |
1766195070179999744 |