Barotropic tides of the Southern Indian Ocean and the Amery Ice Shelf cavity

The 8 main tidal constituents were computed using a finite element, hydrodynamic ocean tide model over the South Indian Ocean region. The discretization of the domain is of the order of 100 km over the deep ocean and a few hundred meters near the coast. Such refinement in the grid resolution enables...

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Published in:Geophysical Research Letters
Main Authors: Maraldi, C, Galton-Fenzi, BK, Lyard, F, Testut, L, Coleman, R
Format: Article in Journal/Newspaper
Language:English
Published: 2007
Subjects:
Online Access:https://eprints.utas.edu.au/6998/
https://eprints.utas.edu.au/6998/1/Maraldi_etal_2007GL030900.pdf
https://doi.org/10.1029/2007GL030900
id ftunivtasmania:oai:eprints.utas.edu.au:6998
record_format openpolar
spelling ftunivtasmania:oai:eprints.utas.edu.au:6998 2023-05-15T13:21:58+02:00 Barotropic tides of the Southern Indian Ocean and the Amery Ice Shelf cavity Maraldi, C Galton-Fenzi, BK Lyard, F Testut, L Coleman, R 2007 application/pdf https://eprints.utas.edu.au/6998/ https://eprints.utas.edu.au/6998/1/Maraldi_etal_2007GL030900.pdf https://doi.org/10.1029/2007GL030900 en eng https://eprints.utas.edu.au/6998/1/Maraldi_etal_2007GL030900.pdf Maraldi, C, Galton-Fenzi, BK, Lyard, F, Testut, L and Coleman, R 2007 , 'Barotropic tides of the Southern Indian Ocean and the Amery Ice Shelf cavity' , Geophysical Research Letters, vol. 34, no. L18602 , pp. 1-5 , doi:10.1029/2007GL030900 <http://dx.doi.org/10.1029/2007GL030900>. cc_utas Indian Ocean Amery Ice Shelf barotropic tides Article PeerReviewed 2007 ftunivtasmania https://doi.org/10.1029/2007GL030900 2020-05-30T07:20:49Z The 8 main tidal constituents were computed using a finite element, hydrodynamic ocean tide model over the South Indian Ocean region. The discretization of the domain is of the order of 100 km over the deep ocean and a few hundred meters near the coast. Such refinement in the grid resolution enables wave propagation and damping on the continental shelves to be solved correctly. The model used the GEBCO 1-minute global bathymetric grid which was improved with updated topographic data. The model solutions show good agreement with in-situ observations and Topex-Poseidon altimeter measurements and are significantly better than previously published solutions. We obtain a combined standard deviation of 1.4 cm for differences of our new regional model against independent observations compared to about 2.5 cm for the other tide models. The greatest improvements are found around the Kerguelen Islands, around Antarctica and beneath the Amery Ice Shelf and can be explained by the high grid resolution used and the particular attention given to the accuracy of the bathymetry in those regions. Article in Journal/Newspaper Amery Ice Shelf Antarc* Antarctica Ice Shelf Kerguelen Islands University of Tasmania: UTas ePrints Kerguelen Kerguelen Islands Indian Amery ENVELOPE(-94.063,-94.063,56.565,56.565) Amery Ice Shelf ENVELOPE(71.000,71.000,-69.750,-69.750) Geophysical Research Letters 34 18
institution Open Polar
collection University of Tasmania: UTas ePrints
op_collection_id ftunivtasmania
language English
topic Indian Ocean
Amery Ice Shelf
barotropic tides
spellingShingle Indian Ocean
Amery Ice Shelf
barotropic tides
Maraldi, C
Galton-Fenzi, BK
Lyard, F
Testut, L
Coleman, R
Barotropic tides of the Southern Indian Ocean and the Amery Ice Shelf cavity
topic_facet Indian Ocean
Amery Ice Shelf
barotropic tides
description The 8 main tidal constituents were computed using a finite element, hydrodynamic ocean tide model over the South Indian Ocean region. The discretization of the domain is of the order of 100 km over the deep ocean and a few hundred meters near the coast. Such refinement in the grid resolution enables wave propagation and damping on the continental shelves to be solved correctly. The model used the GEBCO 1-minute global bathymetric grid which was improved with updated topographic data. The model solutions show good agreement with in-situ observations and Topex-Poseidon altimeter measurements and are significantly better than previously published solutions. We obtain a combined standard deviation of 1.4 cm for differences of our new regional model against independent observations compared to about 2.5 cm for the other tide models. The greatest improvements are found around the Kerguelen Islands, around Antarctica and beneath the Amery Ice Shelf and can be explained by the high grid resolution used and the particular attention given to the accuracy of the bathymetry in those regions.
format Article in Journal/Newspaper
author Maraldi, C
Galton-Fenzi, BK
Lyard, F
Testut, L
Coleman, R
author_facet Maraldi, C
Galton-Fenzi, BK
Lyard, F
Testut, L
Coleman, R
author_sort Maraldi, C
title Barotropic tides of the Southern Indian Ocean and the Amery Ice Shelf cavity
title_short Barotropic tides of the Southern Indian Ocean and the Amery Ice Shelf cavity
title_full Barotropic tides of the Southern Indian Ocean and the Amery Ice Shelf cavity
title_fullStr Barotropic tides of the Southern Indian Ocean and the Amery Ice Shelf cavity
title_full_unstemmed Barotropic tides of the Southern Indian Ocean and the Amery Ice Shelf cavity
title_sort barotropic tides of the southern indian ocean and the amery ice shelf cavity
publishDate 2007
url https://eprints.utas.edu.au/6998/
https://eprints.utas.edu.au/6998/1/Maraldi_etal_2007GL030900.pdf
https://doi.org/10.1029/2007GL030900
long_lat ENVELOPE(-94.063,-94.063,56.565,56.565)
ENVELOPE(71.000,71.000,-69.750,-69.750)
geographic Kerguelen
Kerguelen Islands
Indian
Amery
Amery Ice Shelf
geographic_facet Kerguelen
Kerguelen Islands
Indian
Amery
Amery Ice Shelf
genre Amery Ice Shelf
Antarc*
Antarctica
Ice Shelf
Kerguelen Islands
genre_facet Amery Ice Shelf
Antarc*
Antarctica
Ice Shelf
Kerguelen Islands
op_relation https://eprints.utas.edu.au/6998/1/Maraldi_etal_2007GL030900.pdf
Maraldi, C, Galton-Fenzi, BK, Lyard, F, Testut, L and Coleman, R 2007 , 'Barotropic tides of the Southern Indian Ocean and the Amery Ice Shelf cavity' , Geophysical Research Letters, vol. 34, no. L18602 , pp. 1-5 , doi:10.1029/2007GL030900 <http://dx.doi.org/10.1029/2007GL030900>.
op_rights cc_utas
op_doi https://doi.org/10.1029/2007GL030900
container_title Geophysical Research Letters
container_volume 34
container_issue 18
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