The cavity under the Amery Ice Shelf, East Antarctica

Ocean circulation under ice shelves and associated rates of melting and freezing are strongly influenced by the shape of the sub-ice-shelf cavity. We have refined an existing method and used additional in situ measurements to estimate the cavity shape under the Amery Ice Shelf, East Antarctica. A fi...

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Main Authors: Galton-Fenzi, BK, Maraldi, C, Coleman, R, Hunter, J
Format: Article in Journal/Newspaper
Language:English
Published: 2008
Subjects:
Online Access:https://eprints.utas.edu.au/8443/
https://eprints.utas.edu.au/8443/1/Galton-Fenzi_etal_JGlac_2008.pdf
http://www.igsoc.org/journal/54/188/t08J021.pdf
id ftunivtasmania:oai:eprints.utas.edu.au:8443
record_format openpolar
spelling ftunivtasmania:oai:eprints.utas.edu.au:8443 2023-05-15T13:21:57+02:00 The cavity under the Amery Ice Shelf, East Antarctica Galton-Fenzi, BK Maraldi, C Coleman, R Hunter, J 2008 application/pdf https://eprints.utas.edu.au/8443/ https://eprints.utas.edu.au/8443/1/Galton-Fenzi_etal_JGlac_2008.pdf http://www.igsoc.org/journal/54/188/t08J021.pdf en eng https://eprints.utas.edu.au/8443/1/Galton-Fenzi_etal_JGlac_2008.pdf Galton-Fenzi, BK, Maraldi, C, Coleman, R and Hunter, J 2008 , 'The cavity under the Amery Ice Shelf, East Antarctica' , Journal of Glaciology, vol. 54, no. 188 , pp. 881-887 . cc_utas Amery Ice Shelf East Antarctica physical oceanography sub-ice-shelf cavity ocean circulation Article PeerReviewed 2008 ftunivtasmania 2020-05-30T07:22:12Z Ocean circulation under ice shelves and associated rates of melting and freezing are strongly influenced by the shape of the sub-ice-shelf cavity. We have refined an existing method and used additional in situ measurements to estimate the cavity shape under the Amery Ice Shelf, East Antarctica. A finite-element hydrodynamic ocean-tide model was used to simulate the major tidal constituents for a range of different sub-Amery Ice Shelf cavity water-column thicknesses. The data are adjusted in the largely unsurveyed southern region of the ice-shelf cavity by comparing the complex error between simulated tides and in situ tides, derived from GPS observations. We show a significant improvement in the simulated tides, with a combined complex error of 1.8 cm, in comparison with past studies which show a complex error of ∼5.3 cm. Our bathymetry incorporates ice-draft data at the grounding line and seismic surveys, which have provided a considerable amount of new data. This technique has particular application when the water column beneath ice shelves is inaccessible and in situ GPS data are available. Article in Journal/Newspaper Amery Ice Shelf Antarc* Antarctica Antarctica Journal East Antarctica Ice Shelf Ice Shelves Journal of Glaciology University of Tasmania: UTas ePrints East Antarctica Amery ENVELOPE(-94.063,-94.063,56.565,56.565) Amery Ice Shelf ENVELOPE(71.000,71.000,-69.750,-69.750)
institution Open Polar
collection University of Tasmania: UTas ePrints
op_collection_id ftunivtasmania
language English
topic Amery Ice Shelf
East Antarctica
physical oceanography
sub-ice-shelf cavity
ocean circulation
spellingShingle Amery Ice Shelf
East Antarctica
physical oceanography
sub-ice-shelf cavity
ocean circulation
Galton-Fenzi, BK
Maraldi, C
Coleman, R
Hunter, J
The cavity under the Amery Ice Shelf, East Antarctica
topic_facet Amery Ice Shelf
East Antarctica
physical oceanography
sub-ice-shelf cavity
ocean circulation
description Ocean circulation under ice shelves and associated rates of melting and freezing are strongly influenced by the shape of the sub-ice-shelf cavity. We have refined an existing method and used additional in situ measurements to estimate the cavity shape under the Amery Ice Shelf, East Antarctica. A finite-element hydrodynamic ocean-tide model was used to simulate the major tidal constituents for a range of different sub-Amery Ice Shelf cavity water-column thicknesses. The data are adjusted in the largely unsurveyed southern region of the ice-shelf cavity by comparing the complex error between simulated tides and in situ tides, derived from GPS observations. We show a significant improvement in the simulated tides, with a combined complex error of 1.8 cm, in comparison with past studies which show a complex error of ∼5.3 cm. Our bathymetry incorporates ice-draft data at the grounding line and seismic surveys, which have provided a considerable amount of new data. This technique has particular application when the water column beneath ice shelves is inaccessible and in situ GPS data are available.
format Article in Journal/Newspaper
author Galton-Fenzi, BK
Maraldi, C
Coleman, R
Hunter, J
author_facet Galton-Fenzi, BK
Maraldi, C
Coleman, R
Hunter, J
author_sort Galton-Fenzi, BK
title The cavity under the Amery Ice Shelf, East Antarctica
title_short The cavity under the Amery Ice Shelf, East Antarctica
title_full The cavity under the Amery Ice Shelf, East Antarctica
title_fullStr The cavity under the Amery Ice Shelf, East Antarctica
title_full_unstemmed The cavity under the Amery Ice Shelf, East Antarctica
title_sort cavity under the amery ice shelf, east antarctica
publishDate 2008
url https://eprints.utas.edu.au/8443/
https://eprints.utas.edu.au/8443/1/Galton-Fenzi_etal_JGlac_2008.pdf
http://www.igsoc.org/journal/54/188/t08J021.pdf
long_lat ENVELOPE(-94.063,-94.063,56.565,56.565)
ENVELOPE(71.000,71.000,-69.750,-69.750)
geographic East Antarctica
Amery
Amery Ice Shelf
geographic_facet East Antarctica
Amery
Amery Ice Shelf
genre Amery Ice Shelf
Antarc*
Antarctica
Antarctica Journal
East Antarctica
Ice Shelf
Ice Shelves
Journal of Glaciology
genre_facet Amery Ice Shelf
Antarc*
Antarctica
Antarctica Journal
East Antarctica
Ice Shelf
Ice Shelves
Journal of Glaciology
op_relation https://eprints.utas.edu.au/8443/1/Galton-Fenzi_etal_JGlac_2008.pdf
Galton-Fenzi, BK, Maraldi, C, Coleman, R and Hunter, J 2008 , 'The cavity under the Amery Ice Shelf, East Antarctica' , Journal of Glaciology, vol. 54, no. 188 , pp. 881-887 .
op_rights cc_utas
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