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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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 |
_version_ |
1766362422084370432 |