Antarctic ice rise formation, evolution, and stability
Antarctic ice rises originate from the contact between ice shelves and one of the numerous topographic highs emerging from the edge of the continental shelf. While investigations of the Raymond effect indicate their millennial-scale stability, little is known about their formation and their role in...
Published in: | Geophysical Research Letters |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2015
|
Subjects: | |
Online Access: | https://www.vliz.be/imisdocs/publications/314076.pdf |
id |
ftvliz:oai:oma.vliz.be:295817 |
---|---|
record_format |
openpolar |
spelling |
ftvliz:oai:oma.vliz.be:295817 2023-05-15T13:54:11+02:00 Antarctic ice rise formation, evolution, and stability Favier, L. Pattyn, F. 2015 application/pdf https://www.vliz.be/imisdocs/publications/314076.pdf en eng info:eu-repo/semantics/altIdentifier/wos/000357511200026 info:eu-repo/semantics/altIdentifier/doi/doi.org/10.1002/2015GL064195 https://www.vliz.be/imisdocs/publications/314076.pdf info:eu-repo/semantics/openAccess %3Ci%3EGeophys.+Res.+Lett.+42%2811%29%3C%2Fi%3E%3A+4456-4463.+%3Ca+href%3D%22https%3A%2F%2Fdx.doi.org%2F10.1002%2F2015GL064195%22+target%3D%22_blank%22%3Ehttps%3A%2F%2Fdx.doi.org%2F10.1002%2F2015GL064195%3C%2Fa%3E info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftvliz https://doi.org/10.1002/2015GL064195 2022-05-01T11:00:14Z Antarctic ice rises originate from the contact between ice shelves and one of the numerous topographic highs emerging from the edge of the continental shelf. While investigations of the Raymond effect indicate their millennial-scale stability, little is known about their formation and their role in ice shelf stability. Here we present for the first time the simulation of an ice rise using the BISICLES model. The numerical results successfully reproduce several field-observable features, such as the substantial thinning downstream of the ice rise and the successive formation of a promontory and ice rise with stable radial ice flow center, showing that ice rises are formed during the ice sheet deglaciation. We quantify the ice rise buttressing effect, found to be mostly transient, delaying grounding line retreat significantly but resulting in comparable steady state positions. We demonstrate that ice rises are key in controlling simulations of Antarctic deglaciation. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Flanders Marine Institute (VLIZ): Open Marine Archive (OMA) Antarctic Geophysical Research Letters 42 11 4456 4463 |
institution |
Open Polar |
collection |
Flanders Marine Institute (VLIZ): Open Marine Archive (OMA) |
op_collection_id |
ftvliz |
language |
English |
description |
Antarctic ice rises originate from the contact between ice shelves and one of the numerous topographic highs emerging from the edge of the continental shelf. While investigations of the Raymond effect indicate their millennial-scale stability, little is known about their formation and their role in ice shelf stability. Here we present for the first time the simulation of an ice rise using the BISICLES model. The numerical results successfully reproduce several field-observable features, such as the substantial thinning downstream of the ice rise and the successive formation of a promontory and ice rise with stable radial ice flow center, showing that ice rises are formed during the ice sheet deglaciation. We quantify the ice rise buttressing effect, found to be mostly transient, delaying grounding line retreat significantly but resulting in comparable steady state positions. We demonstrate that ice rises are key in controlling simulations of Antarctic deglaciation. |
format |
Article in Journal/Newspaper |
author |
Favier, L. Pattyn, F. |
spellingShingle |
Favier, L. Pattyn, F. Antarctic ice rise formation, evolution, and stability |
author_facet |
Favier, L. Pattyn, F. |
author_sort |
Favier, L. |
title |
Antarctic ice rise formation, evolution, and stability |
title_short |
Antarctic ice rise formation, evolution, and stability |
title_full |
Antarctic ice rise formation, evolution, and stability |
title_fullStr |
Antarctic ice rise formation, evolution, and stability |
title_full_unstemmed |
Antarctic ice rise formation, evolution, and stability |
title_sort |
antarctic ice rise formation, evolution, and stability |
publishDate |
2015 |
url |
https://www.vliz.be/imisdocs/publications/314076.pdf |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves |
genre_facet |
Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves |
op_source |
%3Ci%3EGeophys.+Res.+Lett.+42%2811%29%3C%2Fi%3E%3A+4456-4463.+%3Ca+href%3D%22https%3A%2F%2Fdx.doi.org%2F10.1002%2F2015GL064195%22+target%3D%22_blank%22%3Ehttps%3A%2F%2Fdx.doi.org%2F10.1002%2F2015GL064195%3C%2Fa%3E |
op_relation |
info:eu-repo/semantics/altIdentifier/wos/000357511200026 info:eu-repo/semantics/altIdentifier/doi/doi.org/10.1002/2015GL064195 https://www.vliz.be/imisdocs/publications/314076.pdf |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1002/2015GL064195 |
container_title |
Geophysical Research Letters |
container_volume |
42 |
container_issue |
11 |
container_start_page |
4456 |
op_container_end_page |
4463 |
_version_ |
1766259867538948096 |