Glaciation of the central part of the Sør Rondane, Antarctica: glaciological evidence
Ice thickness measurements, carried out by radio echo sounder and gravimeter in the central part of the Sør Rondane Mountains, reveal a subglacial topography of the outlet glaciers and its tributaries characterized by U-shaped valley profiles and overdeepened bedrock. Mass-flux measurements highligh...
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ftvliz:oai:oma.vliz.be:199756 2023-05-15T13:33:15+02:00 Glaciation of the central part of the Sør Rondane, Antarctica: glaciological evidence Pattyn, F. Decleir, H. Huybrechts, P. 1992 http://www.vliz.be/nl/open-marien-archief?module=ref&refid=199756 en eng http://www.vliz.be/nl/open-marien-archief?module=ref&refid=199756 info:eu-repo/semantics/restrictedAccess +biinib+Yoshida+Y.+iet+al.i+iRecent+Progress+in+Antarctic+Earth+Science.+Proceedings+of+the+Sixth+International+Symposium+on+Antarctic+Earth+Sciences+held+at+National+Womens+Education+Centre+Ranzan+Saitama+Japan+September+9-13+1991.i+pp.+669-678 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1992 ftvliz 2022-05-01T09:23:04Z Ice thickness measurements, carried out by radio echo sounder and gravimeter in the central part of the Sør Rondane Mountains, reveal a subglacial topography of the outlet glaciers and its tributaries characterized by U-shaped valley profiles and overdeepened bedrock. Mass-flux measurements highlight the reduced flow of at least one glacier (Jenningsbreen). This glacier is in the process of being cut off from the main ice supply and may serve as an example for the deglaciation process. An interesting feature of this deglaciation is that, once decoupled from the main ice supply, this glacier is probably characterized by an increased lowering of the ice surface gradient due to the ablation which is characteristic for the upper part of the present outlet glacier. In the end this will result in a southward flow of which examples can be found elsewhere in the mountains. On the basis of the field evidence a numerical flow line model is presented to simulate the behaviour of the outlet glaciers of the central part of the mountains during the last glacial maximum. These experiments show an increase of 300-400 m in ice thickness under realistic assumptions for mass balance, temperature and sea level. Some of the higher glacial levels are then attributed to an environment characterized by a higher accumulation predating the last glacial maximum. Article in Journal/Newspaper Antarc* Antarctica Flanders Marine Institute (VLIZ): Open Marine Archive (OMA) Jenningsbreen ENVELOPE(24.367,24.367,-71.950,-71.950) Sør Rondane Mountains ENVELOPE(25.000,25.000,-72.000,-72.000) Sør-Rondane ENVELOPE(25.000,25.000,-72.000,-72.000) |
institution |
Open Polar |
collection |
Flanders Marine Institute (VLIZ): Open Marine Archive (OMA) |
op_collection_id |
ftvliz |
language |
English |
description |
Ice thickness measurements, carried out by radio echo sounder and gravimeter in the central part of the Sør Rondane Mountains, reveal a subglacial topography of the outlet glaciers and its tributaries characterized by U-shaped valley profiles and overdeepened bedrock. Mass-flux measurements highlight the reduced flow of at least one glacier (Jenningsbreen). This glacier is in the process of being cut off from the main ice supply and may serve as an example for the deglaciation process. An interesting feature of this deglaciation is that, once decoupled from the main ice supply, this glacier is probably characterized by an increased lowering of the ice surface gradient due to the ablation which is characteristic for the upper part of the present outlet glacier. In the end this will result in a southward flow of which examples can be found elsewhere in the mountains. On the basis of the field evidence a numerical flow line model is presented to simulate the behaviour of the outlet glaciers of the central part of the mountains during the last glacial maximum. These experiments show an increase of 300-400 m in ice thickness under realistic assumptions for mass balance, temperature and sea level. Some of the higher glacial levels are then attributed to an environment characterized by a higher accumulation predating the last glacial maximum. |
format |
Article in Journal/Newspaper |
author |
Pattyn, F. Decleir, H. Huybrechts, P. |
spellingShingle |
Pattyn, F. Decleir, H. Huybrechts, P. Glaciation of the central part of the Sør Rondane, Antarctica: glaciological evidence |
author_facet |
Pattyn, F. Decleir, H. Huybrechts, P. |
author_sort |
Pattyn, F. |
title |
Glaciation of the central part of the Sør Rondane, Antarctica: glaciological evidence |
title_short |
Glaciation of the central part of the Sør Rondane, Antarctica: glaciological evidence |
title_full |
Glaciation of the central part of the Sør Rondane, Antarctica: glaciological evidence |
title_fullStr |
Glaciation of the central part of the Sør Rondane, Antarctica: glaciological evidence |
title_full_unstemmed |
Glaciation of the central part of the Sør Rondane, Antarctica: glaciological evidence |
title_sort |
glaciation of the central part of the sør rondane, antarctica: glaciological evidence |
publishDate |
1992 |
url |
http://www.vliz.be/nl/open-marien-archief?module=ref&refid=199756 |
long_lat |
ENVELOPE(24.367,24.367,-71.950,-71.950) ENVELOPE(25.000,25.000,-72.000,-72.000) ENVELOPE(25.000,25.000,-72.000,-72.000) |
geographic |
Jenningsbreen Sør Rondane Mountains Sør-Rondane |
geographic_facet |
Jenningsbreen Sør Rondane Mountains Sør-Rondane |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
+biinib+Yoshida+Y.+iet+al.i+iRecent+Progress+in+Antarctic+Earth+Science.+Proceedings+of+the+Sixth+International+Symposium+on+Antarctic+Earth+Sciences+held+at+National+Womens+Education+Centre+Ranzan+Saitama+Japan+September+9-13+1991.i+pp.+669-678 |
op_relation |
http://www.vliz.be/nl/open-marien-archief?module=ref&refid=199756 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1766040351102992384 |