Three-dimensional reconstruction of oceanic mesoscale currents from surface information

International audience The ability to reconstruct the three‐dimensional (3D) dynamics of the ocean by an effective version of Surface Quasi‐Geostrophy (eSQG) is examined. Using the fact that surface density plays an analogous role as interior potential vorticity (PV), the eSQG method consists in inv...

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Published in:Journal of Geophysical Research
Main Authors: Capet, Xavier, Hua, Bach Lien, Mcwilliams, James C., Isern-Fontanet, Jordi, Lapeyre, Guillaume, Klein, Patrice, Chapron, Bertrand, Hecht, Matthew
Other Authors: Laboratoire de physique des océans (LPO), Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS), Department of Atmospheric Sciences Los Angeles, University of California Los Angeles (UCLA), University of California (UC)-University of California (UC), Laboratoire d'Océanographie Spatiale (LOS), Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER), Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X), Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-École des Ponts ParisTech (ENPC)-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), Los Alamos National Laboratory (LANL)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2008
Subjects:
SST
Online Access:https://hal.science/hal-02051290
https://hal.science/hal-02051290/document
https://hal.science/hal-02051290/file/2007JC004692.pdf
https://doi.org/10.1029/2007JC004692
id ftecoleponts:oai:HAL:hal-02051290v1
record_format openpolar
institution Open Polar
collection École des Ponts ParisTech: HAL
op_collection_id ftecoleponts
language English
topic 3D dynamics reconstruction
SST
Surface Quasi‐Geostrophy
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[PHYS.PHYS.PHYS-FLU-DYN]Physics [physics]/Physics [physics]/Fluid Dynamics [physics.flu-dyn]
spellingShingle 3D dynamics reconstruction
SST
Surface Quasi‐Geostrophy
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[PHYS.PHYS.PHYS-FLU-DYN]Physics [physics]/Physics [physics]/Fluid Dynamics [physics.flu-dyn]
Capet, Xavier
Hua, Bach Lien
Mcwilliams, James C.
Isern-Fontanet, Jordi
Lapeyre, Guillaume
Klein, Patrice
Chapron, Bertrand
Hecht, Matthew
Three-dimensional reconstruction of oceanic mesoscale currents from surface information
topic_facet 3D dynamics reconstruction
SST
Surface Quasi‐Geostrophy
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[PHYS.PHYS.PHYS-FLU-DYN]Physics [physics]/Physics [physics]/Fluid Dynamics [physics.flu-dyn]
description International audience The ability to reconstruct the three‐dimensional (3D) dynamics of the ocean by an effective version of Surface Quasi‐Geostrophy (eSQG) is examined. Using the fact that surface density plays an analogous role as interior potential vorticity (PV), the eSQG method consists in inverting the QG PV generated by sea‐surface density only. We also make the extra assumption that sea‐surface temperature (SST) anomalies fully represent surface density anomalies. This approach requires a single snapshot of SST and the setup of two parameters: the mean Brunt‐Väisälä frequency and a parameter that determines the energy level at the ocean surface. The validity of this approach is tested using an Ocean General Circulation Model simulation representing the North Atlantic in winter. It is shown that the method is quite successful in reconstructing the velocity field at the ocean surface for mesoscales (between 30 and 300 km). The eSQG framework can also be applied to reconstruct subsurface fields using surface information. Results show that the reconstruction of velocities and vorticity from surface fields is reasonably good for the upper 500 m and that the success of the method mainly depends on the quality of the SST as a proxy of the density anomaly at the base of the mixed layer. This situation happens after a mixed‐layer deepening period. Therefore the ideal situation for the application of this method would be after strong wind events.
author2 Laboratoire de physique des océans (LPO)
Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)
Department of Atmospheric Sciences Los Angeles
University of California Los Angeles (UCLA)
University of California (UC)-University of California (UC)
Laboratoire d'Océanographie Spatiale (LOS)
Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)
Laboratoire de Météorologie Dynamique (UMR 8539) (LMD)
Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)
Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-École des Ponts ParisTech (ENPC)-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)
Los Alamos National Laboratory (LANL)
format Article in Journal/Newspaper
author Capet, Xavier
Hua, Bach Lien
Mcwilliams, James C.
Isern-Fontanet, Jordi
Lapeyre, Guillaume
Klein, Patrice
Chapron, Bertrand
Hecht, Matthew
author_facet Capet, Xavier
Hua, Bach Lien
Mcwilliams, James C.
Isern-Fontanet, Jordi
Lapeyre, Guillaume
Klein, Patrice
Chapron, Bertrand
Hecht, Matthew
author_sort Capet, Xavier
title Three-dimensional reconstruction of oceanic mesoscale currents from surface information
title_short Three-dimensional reconstruction of oceanic mesoscale currents from surface information
title_full Three-dimensional reconstruction of oceanic mesoscale currents from surface information
title_fullStr Three-dimensional reconstruction of oceanic mesoscale currents from surface information
title_full_unstemmed Three-dimensional reconstruction of oceanic mesoscale currents from surface information
title_sort three-dimensional reconstruction of oceanic mesoscale currents from surface information
publisher HAL CCSD
publishDate 2008
url https://hal.science/hal-02051290
https://hal.science/hal-02051290/document
https://hal.science/hal-02051290/file/2007JC004692.pdf
https://doi.org/10.1029/2007JC004692
genre North Atlantic
genre_facet North Atlantic
op_source ISSN: 0148-0227
EISSN: 2156-2202
Journal of Geophysical Research
https://hal.science/hal-02051290
Journal of Geophysical Research, 2008, 113 (C9), ⟨10.1029/2007JC004692⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2007JC004692
hal-02051290
https://hal.science/hal-02051290
https://hal.science/hal-02051290/document
https://hal.science/hal-02051290/file/2007JC004692.pdf
doi:10.1029/2007JC004692
op_rights http://hal.archives-ouvertes.fr/licences/copyright/
info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/2007JC004692
container_title Journal of Geophysical Research
container_volume 113
container_issue C9
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spelling ftecoleponts:oai:HAL:hal-02051290v1 2024-09-15T18:24:00+00:00 Three-dimensional reconstruction of oceanic mesoscale currents from surface information Capet, Xavier Hua, Bach Lien Mcwilliams, James C. Isern-Fontanet, Jordi Lapeyre, Guillaume Klein, Patrice Chapron, Bertrand Hecht, Matthew Laboratoire de physique des océans (LPO) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) Department of Atmospheric Sciences Los Angeles University of California Los Angeles (UCLA) University of California (UC)-University of California (UC) Laboratoire d'Océanographie Spatiale (LOS) Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER) Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-École des Ponts ParisTech (ENPC)-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) Los Alamos National Laboratory (LANL) 2008 https://hal.science/hal-02051290 https://hal.science/hal-02051290/document https://hal.science/hal-02051290/file/2007JC004692.pdf https://doi.org/10.1029/2007JC004692 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2007JC004692 hal-02051290 https://hal.science/hal-02051290 https://hal.science/hal-02051290/document https://hal.science/hal-02051290/file/2007JC004692.pdf doi:10.1029/2007JC004692 http://hal.archives-ouvertes.fr/licences/copyright/ info:eu-repo/semantics/OpenAccess ISSN: 0148-0227 EISSN: 2156-2202 Journal of Geophysical Research https://hal.science/hal-02051290 Journal of Geophysical Research, 2008, 113 (C9), ⟨10.1029/2007JC004692⟩ 3D dynamics reconstruction SST Surface Quasi‐Geostrophy [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] [PHYS.PHYS.PHYS-FLU-DYN]Physics [physics]/Physics [physics]/Fluid Dynamics [physics.flu-dyn] info:eu-repo/semantics/article Journal articles 2008 ftecoleponts https://doi.org/10.1029/2007JC004692 2024-08-13T23:47:27Z International audience The ability to reconstruct the three‐dimensional (3D) dynamics of the ocean by an effective version of Surface Quasi‐Geostrophy (eSQG) is examined. Using the fact that surface density plays an analogous role as interior potential vorticity (PV), the eSQG method consists in inverting the QG PV generated by sea‐surface density only. We also make the extra assumption that sea‐surface temperature (SST) anomalies fully represent surface density anomalies. This approach requires a single snapshot of SST and the setup of two parameters: the mean Brunt‐Väisälä frequency and a parameter that determines the energy level at the ocean surface. The validity of this approach is tested using an Ocean General Circulation Model simulation representing the North Atlantic in winter. It is shown that the method is quite successful in reconstructing the velocity field at the ocean surface for mesoscales (between 30 and 300 km). The eSQG framework can also be applied to reconstruct subsurface fields using surface information. Results show that the reconstruction of velocities and vorticity from surface fields is reasonably good for the upper 500 m and that the success of the method mainly depends on the quality of the SST as a proxy of the density anomaly at the base of the mixed layer. This situation happens after a mixed‐layer deepening period. Therefore the ideal situation for the application of this method would be after strong wind events. Article in Journal/Newspaper North Atlantic École des Ponts ParisTech: HAL Journal of Geophysical Research 113 C9