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...
Main Authors: | , , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2008
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Online Access: | https://figshare.com/articles/journal_contribution/The_cavity_under_the_Amery_Ice_Shelf_East_Antarctica/23227319 |
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author | Galton-Fenzi, BK Maraldi, C Richard Coleman John Hunter |
author_facet | Galton-Fenzi, BK Maraldi, C Richard Coleman John Hunter |
author_sort | Galton-Fenzi, BK |
collection | Research from University Of Tasmania |
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 ‚Äöv†¬¿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 |
genre | Amery Ice Shelf Antarc* Antarctica East Antarctica Ice Shelf Ice Shelves |
genre_facet | Amery Ice Shelf Antarc* Antarctica East Antarctica Ice Shelf Ice Shelves |
geographic | Amery Amery Ice Shelf East Antarctica |
geographic_facet | Amery Amery Ice Shelf East Antarctica |
id | ftunivtasmanfig:oai:figshare.com:article/23227319 |
institution | Open Polar |
language | unknown |
long_lat | ENVELOPE(-94.063,-94.063,56.565,56.565) ENVELOPE(71.000,71.000,-69.750,-69.750) |
op_collection_id | ftunivtasmanfig |
op_relation | 102.100.100/491207 https://figshare.com/articles/journal_contribution/The_cavity_under_the_Amery_Ice_Shelf_East_Antarctica/23227319 |
op_rights | In Copyright |
publishDate | 2008 |
record_format | openpolar |
spelling | ftunivtasmanfig:oai:figshare.com:article/23227319 2025-03-16T15:15:44+00:00 The cavity under the Amery Ice Shelf, East Antarctica Galton-Fenzi, BK Maraldi, C Richard Coleman John Hunter 2008-01-01T00:00:00Z https://figshare.com/articles/journal_contribution/The_cavity_under_the_Amery_Ice_Shelf_East_Antarctica/23227319 unknown 102.100.100/491207 https://figshare.com/articles/journal_contribution/The_cavity_under_the_Amery_Ice_Shelf_East_Antarctica/23227319 In Copyright Amery Ice Shelf East Antarctica physical oceanography sub-ice-shelf cavity ocean circulation Text Journal contribution 2008 ftunivtasmanfig 2025-02-17T09:48:20Z 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 ‚Äöv†¬¿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 East Antarctica Ice Shelf Ice Shelves Research from University Of Tasmania Amery ENVELOPE(-94.063,-94.063,56.565,56.565) Amery Ice Shelf ENVELOPE(71.000,71.000,-69.750,-69.750) East Antarctica |
spellingShingle | Amery Ice Shelf East Antarctica physical oceanography sub-ice-shelf cavity ocean circulation Galton-Fenzi, BK Maraldi, C Richard Coleman John Hunter The cavity under the Amery Ice Shelf, East Antarctica |
title | 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_short | The cavity under the Amery Ice Shelf, East Antarctica |
title_sort | cavity under the amery ice shelf, east antarctica |
topic | Amery Ice Shelf East Antarctica physical oceanography sub-ice-shelf cavity ocean circulation |
topic_facet | Amery Ice Shelf East Antarctica physical oceanography sub-ice-shelf cavity ocean circulation |
url | https://figshare.com/articles/journal_contribution/The_cavity_under_the_Amery_Ice_Shelf_East_Antarctica/23227319 |