Determination of the surface geostrophic velocity field from satellite altimetry
Presently available marine geoid models are not accurate enough to extract the mean surface circulation directly from satellite altimetry. A novel method for estimating the mean velocity field of major ocean current systems is derived from the free surface boundary condition. With a given quasi-geos...
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ftmuseumnhn:oai:HAL:hal-00164938v1 2023-07-30T04:07:04+02:00 Determination of the surface geostrophic velocity field from satellite altimetry Park, Young-Hyang Département Milieux et Peuplements Aquatiques Muséum national d'Histoire naturelle (MNHN) 2004 https://hal.science/hal-00164938 https://hal.science/hal-00164938/document https://hal.science/hal-00164938/file/2003JC002115.pdf https://doi.org/10.1029/2003JC002115 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2003JC002115 hal-00164938 https://hal.science/hal-00164938 https://hal.science/hal-00164938/document https://hal.science/hal-00164938/file/2003JC002115.pdf doi:10.1029/2003JC002115 info:eu-repo/semantics/OpenAccess ISSN: 0148-0227 EISSN: 2156-2202 Journal of Geophysical Research https://hal.science/hal-00164938 Journal of Geophysical Research, 2004, 109, pp.C05006. ⟨10.1029/2003JC002115⟩ altimetry method velocity field [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2004 ftmuseumnhn https://doi.org/10.1029/2003JC002115 2023-07-08T20:28:13Z Presently available marine geoid models are not accurate enough to extract the mean surface circulation directly from satellite altimetry. A novel method for estimating the mean velocity field of major ocean current systems is derived from the free surface boundary condition. With a given quasi-geostrophic balance for the horizontal surface flow, a scaling analysis of this boundary condition indicates that although the vertical velocity w is mostly balanced by the local change of the free surface, ∂η′/∂t, useful information on the mean current ($\bar{u}$, $\bar{v}$) is contained in a small ageostrophic departure (∂η′/∂t − w). Our method consists in the development of a simple algebraic equation with two unknowns ($\bar{u}$, $\bar{v}$) and an adjustable parameter $\tilde{\alpha}$ associated with ∂η′/∂t, assuming that the latter is proportional to (∂η′/∂t − w). Most interestingly, ∂η′/∂t and all other coefficients of the equation can be determined from altimetry. The altimeter data used is combined TOPEX/Poseidon-ERS gridded data, and the solution is obtained by least squares, minimizing the contribution from the time-variable part of the parameter $\tilde{\alpha}$ and prescribing the zonal direction of the mean current. The method, which is found to be particularly useful for quasi-zonal high-energy current systems, has been validated against direct observations in the Gulf Stream and Southern Ocean. Comparisons with direct observations and Monte Carlo experiments suggest an overall solution error of about 10 cm s −1 . Once calibrated against regional velocity statistics, this method will be able to determine from altimetry the mean or instantaneous surface velocity field down to the frontal scale, with a realism that has been inaccessible because of the geoid constraint. Article in Journal/Newspaper Southern Ocean Muséum National d'Histoire Naturelle (MNHM): HAL Southern Ocean Journal of Geophysical Research 109 C5 |
institution |
Open Polar |
collection |
Muséum National d'Histoire Naturelle (MNHM): HAL |
op_collection_id |
ftmuseumnhn |
language |
English |
topic |
altimetry method velocity field [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
altimetry method velocity field [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [SDE.MCG]Environmental Sciences/Global Changes Park, Young-Hyang Determination of the surface geostrophic velocity field from satellite altimetry |
topic_facet |
altimetry method velocity field [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [SDE.MCG]Environmental Sciences/Global Changes |
description |
Presently available marine geoid models are not accurate enough to extract the mean surface circulation directly from satellite altimetry. A novel method for estimating the mean velocity field of major ocean current systems is derived from the free surface boundary condition. With a given quasi-geostrophic balance for the horizontal surface flow, a scaling analysis of this boundary condition indicates that although the vertical velocity w is mostly balanced by the local change of the free surface, ∂η′/∂t, useful information on the mean current ($\bar{u}$, $\bar{v}$) is contained in a small ageostrophic departure (∂η′/∂t − w). Our method consists in the development of a simple algebraic equation with two unknowns ($\bar{u}$, $\bar{v}$) and an adjustable parameter $\tilde{\alpha}$ associated with ∂η′/∂t, assuming that the latter is proportional to (∂η′/∂t − w). Most interestingly, ∂η′/∂t and all other coefficients of the equation can be determined from altimetry. The altimeter data used is combined TOPEX/Poseidon-ERS gridded data, and the solution is obtained by least squares, minimizing the contribution from the time-variable part of the parameter $\tilde{\alpha}$ and prescribing the zonal direction of the mean current. The method, which is found to be particularly useful for quasi-zonal high-energy current systems, has been validated against direct observations in the Gulf Stream and Southern Ocean. Comparisons with direct observations and Monte Carlo experiments suggest an overall solution error of about 10 cm s −1 . Once calibrated against regional velocity statistics, this method will be able to determine from altimetry the mean or instantaneous surface velocity field down to the frontal scale, with a realism that has been inaccessible because of the geoid constraint. |
author2 |
Département Milieux et Peuplements Aquatiques Muséum national d'Histoire naturelle (MNHN) |
format |
Article in Journal/Newspaper |
author |
Park, Young-Hyang |
author_facet |
Park, Young-Hyang |
author_sort |
Park, Young-Hyang |
title |
Determination of the surface geostrophic velocity field from satellite altimetry |
title_short |
Determination of the surface geostrophic velocity field from satellite altimetry |
title_full |
Determination of the surface geostrophic velocity field from satellite altimetry |
title_fullStr |
Determination of the surface geostrophic velocity field from satellite altimetry |
title_full_unstemmed |
Determination of the surface geostrophic velocity field from satellite altimetry |
title_sort |
determination of the surface geostrophic velocity field from satellite altimetry |
publisher |
HAL CCSD |
publishDate |
2004 |
url |
https://hal.science/hal-00164938 https://hal.science/hal-00164938/document https://hal.science/hal-00164938/file/2003JC002115.pdf https://doi.org/10.1029/2003JC002115 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
ISSN: 0148-0227 EISSN: 2156-2202 Journal of Geophysical Research https://hal.science/hal-00164938 Journal of Geophysical Research, 2004, 109, pp.C05006. ⟨10.1029/2003JC002115⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2003JC002115 hal-00164938 https://hal.science/hal-00164938 https://hal.science/hal-00164938/document https://hal.science/hal-00164938/file/2003JC002115.pdf doi:10.1029/2003JC002115 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2003JC002115 |
container_title |
Journal of Geophysical Research |
container_volume |
109 |
container_issue |
C5 |
_version_ |
1772820166644596736 |