An energetics study of wintertime Northern Hemisphere storm tracks under 4 × CO$_2$ conditions in two ocean–atmosphere coupled models

International audience Different possible behaviors of winter Northern Hemisphere storm tracks under 4 × CO$_2$ forcing are considered by analyzing the response of two of the ocean–atmosphere coupled models that were run for the fourth Assessment Report of the Intergovernmental Panel on Climate Chan...

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Published in:Journal of Climate
Main Authors: Laine, Alexandre, Kageyama, Masa, Salas-Mélia, David, Ramstein, Gilles, Planton, Serge, Denvil, Sébastien, Tyteca, Sophie
Other Authors: Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Modélisation du climat (CLIM), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Centre national de recherches météorologiques (CNRM), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-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)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-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-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL), ANR-05-BLAN-0310,IDEGLACE,Impact de Décharges d'Eau douce provenant de la GLace continentale sur le Climat Européen et méditerranéen(2005)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2009
Subjects:
Online Access:https://hal.science/hal-02930820
https://hal.science/hal-02930820/document
https://hal.science/hal-02930820/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20An%20Energetics%20Study%20of%20Wintertime%20Northern%20Hemisphere%20Storm%20Tracks%20under%204%20%C3%97%20CO2%20Conditions%20in%20Two%20Ocean%E2%80%93Atmosphere%20Coupled%20Models.pdf
https://doi.org/10.1175/2008JCLI2217.1
id ftmeteofrance:oai:HAL:hal-02930820v1
record_format openpolar
institution Open Polar
collection Météo-France: HAL
op_collection_id ftmeteofrance
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
Laine, Alexandre
Kageyama, Masa
Salas-Mélia, David
Ramstein, Gilles
Planton, Serge
Denvil, Sébastien
Tyteca, Sophie
An energetics study of wintertime Northern Hemisphere storm tracks under 4 × CO$_2$ conditions in two ocean–atmosphere coupled models
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
description International audience Different possible behaviors of winter Northern Hemisphere storm tracks under 4 × CO$_2$ forcing are considered by analyzing the response of two of the ocean–atmosphere coupled models that were run for the fourth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC-AR4), namely the Institut Pierre Simon Laplace’s global coupled model (IPSL-CM4) and the Centre National de Recherches Meteorologiques’s coupled ocean–atmosphere model (CNRM-CM3). It is interesting to compare these models due to their very different responses, especially concerning the North Atlantic storm track.A local energetics study of the synoptic variability in both models is performed, derived from the eddy energy equations, including diabatic terms. The ability of both models to simulate the present-day eddy energetics is considered, indicating no major discrepancies.Both models indicate that the primary cause for synoptic activity changes at the western end of the storm tracks is related to the baroclinic conversion process, due to mean temperature gradient changes in some localized regions of the western oceanic basins, but also resulting from changes in the eddy efficiency to convert energy from the mean flow. Farther downstream, latent heat release during the developing and mature stages of eddies becomes an important eddy energy source especially in terms of changes between 4 × CO$_2$ and preindustrial conditions. This diabatic process amplifies the upstream synoptic (hence usually baroclinic) changes, with more and/or stronger storms implying more latent heat being released (and the converse being true for weaker synoptic activity). This amplification is asymmetrical for the models considered under the simulated 4 × CO$_2$ conditions, due to a greater amount of water vapor contained in warmer air and hence the potential for more condensation for a given synoptic activity. The magnitude of the reduced latent heating is attenuated, whereas increased latent heating is strengthened. Ageostrophic ...
author2 Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
Modélisation du climat (CLIM)
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Centre national de recherches météorologiques (CNRM)
Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-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)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-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-Centre National de la Recherche Scientifique (CNRS)
Laboratoire de Météorologie Dynamique (UMR 8539) (LMD)
Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris
École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)
ANR-05-BLAN-0310,IDEGLACE,Impact de Décharges d'Eau douce provenant de la GLace continentale sur le Climat Européen et méditerranéen(2005)
format Article in Journal/Newspaper
author Laine, Alexandre
Kageyama, Masa
Salas-Mélia, David
Ramstein, Gilles
Planton, Serge
Denvil, Sébastien
Tyteca, Sophie
author_facet Laine, Alexandre
Kageyama, Masa
Salas-Mélia, David
Ramstein, Gilles
Planton, Serge
Denvil, Sébastien
Tyteca, Sophie
author_sort Laine, Alexandre
title An energetics study of wintertime Northern Hemisphere storm tracks under 4 × CO$_2$ conditions in two ocean–atmosphere coupled models
title_short An energetics study of wintertime Northern Hemisphere storm tracks under 4 × CO$_2$ conditions in two ocean–atmosphere coupled models
title_full An energetics study of wintertime Northern Hemisphere storm tracks under 4 × CO$_2$ conditions in two ocean–atmosphere coupled models
title_fullStr An energetics study of wintertime Northern Hemisphere storm tracks under 4 × CO$_2$ conditions in two ocean–atmosphere coupled models
title_full_unstemmed An energetics study of wintertime Northern Hemisphere storm tracks under 4 × CO$_2$ conditions in two ocean–atmosphere coupled models
title_sort energetics study of wintertime northern hemisphere storm tracks under 4 × co$_2$ conditions in two ocean–atmosphere coupled models
publisher HAL CCSD
publishDate 2009
url https://hal.science/hal-02930820
https://hal.science/hal-02930820/document
https://hal.science/hal-02930820/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20An%20Energetics%20Study%20of%20Wintertime%20Northern%20Hemisphere%20Storm%20Tracks%20under%204%20%C3%97%20CO2%20Conditions%20in%20Two%20Ocean%E2%80%93Atmosphere%20Coupled%20Models.pdf
https://doi.org/10.1175/2008JCLI2217.1
genre North Atlantic
genre_facet North Atlantic
op_source ISSN: 0894-8755
EISSN: 1520-0442
Journal of Climate
https://hal.science/hal-02930820
Journal of Climate, 2009, 22 (3), pp.819-839. ⟨10.1175/2008JCLI2217.1⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1175/2008JCLI2217.1
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container_title Journal of Climate
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spelling ftmeteofrance:oai:HAL:hal-02930820v1 2024-06-09T07:48:20+00:00 An energetics study of wintertime Northern Hemisphere storm tracks under 4 × CO$_2$ conditions in two ocean–atmosphere coupled models Laine, Alexandre Kageyama, Masa Salas-Mélia, David Ramstein, Gilles Planton, Serge Denvil, Sébastien Tyteca, Sophie Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Modélisation du climat (CLIM) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Centre national de recherches météorologiques (CNRM) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-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)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-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-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) ANR-05-BLAN-0310,IDEGLACE,Impact de Décharges d'Eau douce provenant de la GLace continentale sur le Climat Européen et méditerranéen(2005) 2009 https://hal.science/hal-02930820 https://hal.science/hal-02930820/document https://hal.science/hal-02930820/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20An%20Energetics%20Study%20of%20Wintertime%20Northern%20Hemisphere%20Storm%20Tracks%20under%204%20%C3%97%20CO2%20Conditions%20in%20Two%20Ocean%E2%80%93Atmosphere%20Coupled%20Models.pdf https://doi.org/10.1175/2008JCLI2217.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/2008JCLI2217.1 hal-02930820 https://hal.science/hal-02930820 https://hal.science/hal-02930820/document https://hal.science/hal-02930820/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20An%20Energetics%20Study%20of%20Wintertime%20Northern%20Hemisphere%20Storm%20Tracks%20under%204%20%C3%97%20CO2%20Conditions%20in%20Two%20Ocean%E2%80%93Atmosphere%20Coupled%20Models.pdf doi:10.1175/2008JCLI2217.1 info:eu-repo/semantics/OpenAccess ISSN: 0894-8755 EISSN: 1520-0442 Journal of Climate https://hal.science/hal-02930820 Journal of Climate, 2009, 22 (3), pp.819-839. ⟨10.1175/2008JCLI2217.1⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2009 ftmeteofrance https://doi.org/10.1175/2008JCLI2217.1 2024-05-16T11:50:35Z International audience Different possible behaviors of winter Northern Hemisphere storm tracks under 4 × CO$_2$ forcing are considered by analyzing the response of two of the ocean–atmosphere coupled models that were run for the fourth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC-AR4), namely the Institut Pierre Simon Laplace’s global coupled model (IPSL-CM4) and the Centre National de Recherches Meteorologiques’s coupled ocean–atmosphere model (CNRM-CM3). It is interesting to compare these models due to their very different responses, especially concerning the North Atlantic storm track.A local energetics study of the synoptic variability in both models is performed, derived from the eddy energy equations, including diabatic terms. The ability of both models to simulate the present-day eddy energetics is considered, indicating no major discrepancies.Both models indicate that the primary cause for synoptic activity changes at the western end of the storm tracks is related to the baroclinic conversion process, due to mean temperature gradient changes in some localized regions of the western oceanic basins, but also resulting from changes in the eddy efficiency to convert energy from the mean flow. Farther downstream, latent heat release during the developing and mature stages of eddies becomes an important eddy energy source especially in terms of changes between 4 × CO$_2$ and preindustrial conditions. This diabatic process amplifies the upstream synoptic (hence usually baroclinic) changes, with more and/or stronger storms implying more latent heat being released (and the converse being true for weaker synoptic activity). This amplification is asymmetrical for the models considered under the simulated 4 × CO$_2$ conditions, due to a greater amount of water vapor contained in warmer air and hence the potential for more condensation for a given synoptic activity. The magnitude of the reduced latent heating is attenuated, whereas increased latent heating is strengthened. Ageostrophic ... Article in Journal/Newspaper North Atlantic Météo-France: HAL Journal of Climate 22 3 819 839