Modal Decay in the Australia-Antarctic Basin

International audience The barotropic intraseasonal variability in the Australia–Antarctic Basin (AAB) is studied in terms of the excitation and decay of topographically trapped barotropic modes. The main objective is to reconcile two widely differing estimates of the decay rate of sea surface heigh...

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Published in:Journal of Physical Oceanography
Main Authors: Weijer, Wilbert, Gille, Sarah T., Vivier, Frédéric
Other Authors: Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2009
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-00763287
https://hal.archives-ouvertes.fr/hal-00763287/document
https://hal.archives-ouvertes.fr/hal-00763287/file/%5B15200485%20-%20Journal%20of%20Physical%20Oceanography%5D%20Modal%20Decay%20in%20the%20Australia%E2%80%93Antarctic%20Basin.pdf
https://doi.org/10.1175/2009JPO4209.1
id ftccsdartic:oai:HAL:hal-00763287v1
record_format openpolar
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
spellingShingle [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
Weijer, Wilbert
Gille, Sarah T.
Vivier, Frédéric
Modal Decay in the Australia-Antarctic Basin
topic_facet [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
description International audience The barotropic intraseasonal variability in the Australia–Antarctic Basin (AAB) is studied in terms of the excitation and decay of topographically trapped barotropic modes. The main objective is to reconcile two widely differing estimates of the decay rate of sea surface height (SSH) anomalies in the AAB that are assumed to be related to barotropic modes. First, an empirical orthogonal function (EOF) analysis is applied to almost 15 years of altimeter data. The analysis suggests that several modes are involved in the variability of the AAB, each related to distinct areas with (almost) closed contours of potential vorticity. Second, the dominant normal modes of the AAB are determined in a barotropic shallow-water (SW) model. These stationary modes are confined by the closed contours of potential vorticity that surround the eastern AAB, and the crest of the Southeast Indian Ridge. For reasonable values of horizontal eddy viscosity and bottom friction, their decay time scale is on the order of several weeks. Third, the SW model is forced with realistic winds and integrated for several years. Projection of the modal velocity patterns onto the output fields shows that the barotropic modes are indeed excited in the model, and that they decay slowly on the frictional O(3 weeks) time scale. However, the SSH anomalies in the modal areas display rapid O(4 days) decay. Additional analysis shows that this rapid decay reflects the adjustment of unbalanced flow components through the emission of Rossby waves. Resonant excitation of the dominant free modes accounts for about 20% of the SSH variability in the forced-model run. Other mechanisms are suggested to explain the region of high SSH variability in the AAB.
author2 Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN)
Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636))
École normale supérieure - Paris (ENS Paris)
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS Paris)
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Weijer, Wilbert
Gille, Sarah T.
Vivier, Frédéric
author_facet Weijer, Wilbert
Gille, Sarah T.
Vivier, Frédéric
author_sort Weijer, Wilbert
title Modal Decay in the Australia-Antarctic Basin
title_short Modal Decay in the Australia-Antarctic Basin
title_full Modal Decay in the Australia-Antarctic Basin
title_fullStr Modal Decay in the Australia-Antarctic Basin
title_full_unstemmed Modal Decay in the Australia-Antarctic Basin
title_sort modal decay in the australia-antarctic basin
publisher HAL CCSD
publishDate 2009
url https://hal.archives-ouvertes.fr/hal-00763287
https://hal.archives-ouvertes.fr/hal-00763287/document
https://hal.archives-ouvertes.fr/hal-00763287/file/%5B15200485%20-%20Journal%20of%20Physical%20Oceanography%5D%20Modal%20Decay%20in%20the%20Australia%E2%80%93Antarctic%20Basin.pdf
https://doi.org/10.1175/2009JPO4209.1
long_lat ENVELOPE(110.000,110.000,-50.000,-50.000)
geographic Antarctic
Indian
Southeast Indian Ridge
geographic_facet Antarctic
Indian
Southeast Indian Ridge
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source ISSN: 0022-3670
EISSN: 1520-0485
Journal of Physical Oceanography
https://hal.archives-ouvertes.fr/hal-00763287
Journal of Physical Oceanography, American Meteorological Society, 2009, 39 (11), pp.2893. ⟨10.1175/2009JPO4209.1⟩
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hal-00763287
https://hal.archives-ouvertes.fr/hal-00763287
https://hal.archives-ouvertes.fr/hal-00763287/document
https://hal.archives-ouvertes.fr/hal-00763287/file/%5B15200485%20-%20Journal%20of%20Physical%20Oceanography%5D%20Modal%20Decay%20in%20the%20Australia%E2%80%93Antarctic%20Basin.pdf
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doi:10.1175/2009JPO4209.1
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container_title Journal of Physical Oceanography
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spelling ftccsdartic:oai:HAL:hal-00763287v1 2023-05-15T13:35:08+02:00 Modal Decay in the Australia-Antarctic Basin Weijer, Wilbert Gille, Sarah T. Vivier, Frédéric Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) 2009 https://hal.archives-ouvertes.fr/hal-00763287 https://hal.archives-ouvertes.fr/hal-00763287/document https://hal.archives-ouvertes.fr/hal-00763287/file/%5B15200485%20-%20Journal%20of%20Physical%20Oceanography%5D%20Modal%20Decay%20in%20the%20Australia%E2%80%93Antarctic%20Basin.pdf https://doi.org/10.1175/2009JPO4209.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/2009JPO4209.1 hal-00763287 https://hal.archives-ouvertes.fr/hal-00763287 https://hal.archives-ouvertes.fr/hal-00763287/document https://hal.archives-ouvertes.fr/hal-00763287/file/%5B15200485%20-%20Journal%20of%20Physical%20Oceanography%5D%20Modal%20Decay%20in%20the%20Australia%E2%80%93Antarctic%20Basin.pdf BIBCODE: 2009JPO.39.2893W doi:10.1175/2009JPO4209.1 WOS: 000271912200011 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0022-3670 EISSN: 1520-0485 Journal of Physical Oceanography https://hal.archives-ouvertes.fr/hal-00763287 Journal of Physical Oceanography, American Meteorological Society, 2009, 39 (11), pp.2893. ⟨10.1175/2009JPO4209.1⟩ [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] info:eu-repo/semantics/article Journal articles 2009 ftccsdartic https://doi.org/10.1175/2009JPO4209.1 2021-12-04T23:50:50Z International audience The barotropic intraseasonal variability in the Australia–Antarctic Basin (AAB) is studied in terms of the excitation and decay of topographically trapped barotropic modes. The main objective is to reconcile two widely differing estimates of the decay rate of sea surface height (SSH) anomalies in the AAB that are assumed to be related to barotropic modes. First, an empirical orthogonal function (EOF) analysis is applied to almost 15 years of altimeter data. The analysis suggests that several modes are involved in the variability of the AAB, each related to distinct areas with (almost) closed contours of potential vorticity. Second, the dominant normal modes of the AAB are determined in a barotropic shallow-water (SW) model. These stationary modes are confined by the closed contours of potential vorticity that surround the eastern AAB, and the crest of the Southeast Indian Ridge. For reasonable values of horizontal eddy viscosity and bottom friction, their decay time scale is on the order of several weeks. Third, the SW model is forced with realistic winds and integrated for several years. Projection of the modal velocity patterns onto the output fields shows that the barotropic modes are indeed excited in the model, and that they decay slowly on the frictional O(3 weeks) time scale. However, the SSH anomalies in the modal areas display rapid O(4 days) decay. Additional analysis shows that this rapid decay reflects the adjustment of unbalanced flow components through the emission of Rossby waves. Resonant excitation of the dominant free modes accounts for about 20% of the SSH variability in the forced-model run. Other mechanisms are suggested to explain the region of high SSH variability in the AAB. Article in Journal/Newspaper Antarc* Antarctic Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Antarctic Indian Southeast Indian Ridge ENVELOPE(110.000,110.000,-50.000,-50.000) Journal of Physical Oceanography 39 11 2893 2909