On decadal-scale ocean-atmosphere interactions in the extended ECHAM1/LSG climate simulation
International audience The last 810 years of a control integration with the ECHAM1/LSG coupled model are used to clarify the nature of the ocean-atmosphere interactions at low frequencies in the North Atlantic and the North Pacific. To a first approximation, the atmosphere acts as a white noise forc...
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Online Access: | https://doi.org/10.1007/S003820050332 https://hal.archives-ouvertes.fr/hal-00772172 |
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fttriple:oai:gotriple.eu:10670/1.vguno4 2023-05-15T17:32:06+02:00 On decadal-scale ocean-atmosphere interactions in the extended ECHAM1/LSG climate simulation Frankignoul, Claude Kestenare, Élodie Sennéchael, Nathalie De Coëtlogon, Gaëlle D'Andrea, Fabio Laboratoire d'océanographie dynamique et de climatologie (LODYC) Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC) Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École des Ponts ParisTech (ENPC)-École polytechnique (X)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC) 2000-01-01 https://doi.org/10.1007/S003820050332 https://hal.archives-ouvertes.fr/hal-00772172 en eng HAL CCSD Springer Verlag hal-00772172 BIBCODE: 2000ClDy.16.333F doi:10.1007/S003820050332 10670/1.vguno4 https://hal.archives-ouvertes.fr/hal-00772172 undefined Hyper Article en Ligne - Sciences de l'Homme et de la Société ISSN: 0930-7575 EISSN: 1432-0894 Climate Dynamics Climate Dynamics, Springer Verlag, 2000, 16, pp.333-354. ⟨10.1007/S003820050332⟩ envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2000 fttriple https://doi.org/10.1007/S003820050332 2023-01-22T17:57:27Z International audience The last 810 years of a control integration with the ECHAM1/LSG coupled model are used to clarify the nature of the ocean-atmosphere interactions at low frequencies in the North Atlantic and the North Pacific. To a first approximation, the atmosphere acts as a white noise forcing and the ocean responds as a passive integrator. The sea surface temperature (SST) variability primarily results from short time scale fluctuations in surface heat exchanges and Ekman currents, and the former also damp the SST anomalies after they are generated. The thermocline variability is primarily driven by Ekman pumping. Because the heat, momentum, and vorticity fluxes at the sea surface are correlated in space and time, the SST variability is directly linked to that in the ocean interior. The SST is also modulated by the wind-driven geostrophic fluctuations, resulting in persistent correlation with the thermocline changes and a slight low-frequency redness of the SST spectra. The main dynamics are similar in the two oceans, although in the North Pacific the SST variability is more strongly influenced by advection changes and the oceanic time scales are larger. A maximum covariance analysis based on singular value decomposition in lead and lag conditions indicates that some of the main modes of atmospheric variability in the two oceans are sustained by a very weak positive feedback between the atmosphere, SST, and the strength of the subtropical and subpolar gyres. In addition, in the North Atlantic the main surface pressure mode has a small quasi-oscillatory component at 6-year period, and advective resonance occurs for SST around 10-year period, both periods being also singled out by multichannel singular spectrum analysis. The ocean-atmosphere coupling is however much too weak to redden the tropospheric spectra or create anything more than tiny spectral peaks, so that the atmospheric and oceanic variability is dominated in both ocean sectors by the one-way interactions. Article in Journal/Newspaper North Atlantic Unknown Pacific Climate Dynamics 16 5 333 354 |
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language |
English |
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envir geo |
spellingShingle |
envir geo Frankignoul, Claude Kestenare, Élodie Sennéchael, Nathalie De Coëtlogon, Gaëlle D'Andrea, Fabio On decadal-scale ocean-atmosphere interactions in the extended ECHAM1/LSG climate simulation |
topic_facet |
envir geo |
description |
International audience The last 810 years of a control integration with the ECHAM1/LSG coupled model are used to clarify the nature of the ocean-atmosphere interactions at low frequencies in the North Atlantic and the North Pacific. To a first approximation, the atmosphere acts as a white noise forcing and the ocean responds as a passive integrator. The sea surface temperature (SST) variability primarily results from short time scale fluctuations in surface heat exchanges and Ekman currents, and the former also damp the SST anomalies after they are generated. The thermocline variability is primarily driven by Ekman pumping. Because the heat, momentum, and vorticity fluxes at the sea surface are correlated in space and time, the SST variability is directly linked to that in the ocean interior. The SST is also modulated by the wind-driven geostrophic fluctuations, resulting in persistent correlation with the thermocline changes and a slight low-frequency redness of the SST spectra. The main dynamics are similar in the two oceans, although in the North Pacific the SST variability is more strongly influenced by advection changes and the oceanic time scales are larger. A maximum covariance analysis based on singular value decomposition in lead and lag conditions indicates that some of the main modes of atmospheric variability in the two oceans are sustained by a very weak positive feedback between the atmosphere, SST, and the strength of the subtropical and subpolar gyres. In addition, in the North Atlantic the main surface pressure mode has a small quasi-oscillatory component at 6-year period, and advective resonance occurs for SST around 10-year period, both periods being also singled out by multichannel singular spectrum analysis. The ocean-atmosphere coupling is however much too weak to redden the tropospheric spectra or create anything more than tiny spectral peaks, so that the atmospheric and oceanic variability is dominated in both ocean sectors by the one-way interactions. |
author2 |
Laboratoire d'océanographie dynamique et de climatologie (LODYC) Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC) Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École des Ponts ParisTech (ENPC)-École polytechnique (X)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC) |
format |
Article in Journal/Newspaper |
author |
Frankignoul, Claude Kestenare, Élodie Sennéchael, Nathalie De Coëtlogon, Gaëlle D'Andrea, Fabio |
author_facet |
Frankignoul, Claude Kestenare, Élodie Sennéchael, Nathalie De Coëtlogon, Gaëlle D'Andrea, Fabio |
author_sort |
Frankignoul, Claude |
title |
On decadal-scale ocean-atmosphere interactions in the extended ECHAM1/LSG climate simulation |
title_short |
On decadal-scale ocean-atmosphere interactions in the extended ECHAM1/LSG climate simulation |
title_full |
On decadal-scale ocean-atmosphere interactions in the extended ECHAM1/LSG climate simulation |
title_fullStr |
On decadal-scale ocean-atmosphere interactions in the extended ECHAM1/LSG climate simulation |
title_full_unstemmed |
On decadal-scale ocean-atmosphere interactions in the extended ECHAM1/LSG climate simulation |
title_sort |
on decadal-scale ocean-atmosphere interactions in the extended echam1/lsg climate simulation |
publisher |
HAL CCSD |
publishDate |
2000 |
url |
https://doi.org/10.1007/S003820050332 https://hal.archives-ouvertes.fr/hal-00772172 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Hyper Article en Ligne - Sciences de l'Homme et de la Société ISSN: 0930-7575 EISSN: 1432-0894 Climate Dynamics Climate Dynamics, Springer Verlag, 2000, 16, pp.333-354. ⟨10.1007/S003820050332⟩ |
op_relation |
hal-00772172 BIBCODE: 2000ClDy.16.333F doi:10.1007/S003820050332 10670/1.vguno4 https://hal.archives-ouvertes.fr/hal-00772172 |
op_rights |
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op_doi |
https://doi.org/10.1007/S003820050332 |
container_title |
Climate Dynamics |
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16 |
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5 |
container_start_page |
333 |
op_container_end_page |
354 |
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