Flow Of Antarctic Ice Shelves Between Long. 29° E. And 44° W
This paper discusses the mass outflow and dynamics of a 3000 km long front of the Antarctic ice sheet—the coastline from Prinsesse Ragnhild Kyst to the Filchner Ice Shelf. Ice shelves, mostly 50–100 km wide, account for more than 95% of this coastline. Large mass losses by calving generally occur at...
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Language: | English |
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Cambridge University Press (CUP)
1979
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Online Access: | http://dx.doi.org/10.1017/s0022143000015008 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015008 |
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crcambridgeupr:10.1017/s0022143000015008 2024-03-03T08:37:36+00:00 Flow Of Antarctic Ice Shelves Between Long. 29° E. And 44° W Orheim, Olav 1979 http://dx.doi.org/10.1017/s0022143000015008 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015008 en eng Cambridge University Press (CUP) Journal of Glaciology volume 24, issue 90, page 484-485 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1979 crcambridgeupr https://doi.org/10.1017/s0022143000015008 2024-02-08T08:40:37Z This paper discusses the mass outflow and dynamics of a 3000 km long front of the Antarctic ice sheet—the coastline from Prinsesse Ragnhild Kyst to the Filchner Ice Shelf. Ice shelves, mostly 50–100 km wide, account for more than 95% of this coastline. Large mass losses by calving generally occur at intervals of several decades at any particular location, and usually involve shelf areas of 10-1000 km 2 . The mass loss by calving during the periods between the large calvings is insignificant, except where ice streams run directly into the sea without forming ice shelves. The latter sections account for 2% of the coastline in question and a similar part is made up of ice rises. Thus, with the exception of these short segments, the ice front advances systematically over time intervals of a few decades. Large calvings interrupting the advance can be recognized by significant change in shape and position of the ice front. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Journal of Glaciology Prinsesse Ragnhild Kyst Cambridge University Press Antarctic The Antarctic Filchner Ice Shelf ENVELOPE(-40.000,-40.000,-79.000,-79.000) Prinsesse Ragnhild Kyst ENVELOPE(27.000,27.000,-70.500,-70.500) Journal of Glaciology 24 90 484 485 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Orheim, Olav Flow Of Antarctic Ice Shelves Between Long. 29° E. And 44° W |
topic_facet |
Earth-Surface Processes |
description |
This paper discusses the mass outflow and dynamics of a 3000 km long front of the Antarctic ice sheet—the coastline from Prinsesse Ragnhild Kyst to the Filchner Ice Shelf. Ice shelves, mostly 50–100 km wide, account for more than 95% of this coastline. Large mass losses by calving generally occur at intervals of several decades at any particular location, and usually involve shelf areas of 10-1000 km 2 . The mass loss by calving during the periods between the large calvings is insignificant, except where ice streams run directly into the sea without forming ice shelves. The latter sections account for 2% of the coastline in question and a similar part is made up of ice rises. Thus, with the exception of these short segments, the ice front advances systematically over time intervals of a few decades. Large calvings interrupting the advance can be recognized by significant change in shape and position of the ice front. |
format |
Article in Journal/Newspaper |
author |
Orheim, Olav |
author_facet |
Orheim, Olav |
author_sort |
Orheim, Olav |
title |
Flow Of Antarctic Ice Shelves Between Long. 29° E. And 44° W |
title_short |
Flow Of Antarctic Ice Shelves Between Long. 29° E. And 44° W |
title_full |
Flow Of Antarctic Ice Shelves Between Long. 29° E. And 44° W |
title_fullStr |
Flow Of Antarctic Ice Shelves Between Long. 29° E. And 44° W |
title_full_unstemmed |
Flow Of Antarctic Ice Shelves Between Long. 29° E. And 44° W |
title_sort |
flow of antarctic ice shelves between long. 29° e. and 44° w |
publisher |
Cambridge University Press (CUP) |
publishDate |
1979 |
url |
http://dx.doi.org/10.1017/s0022143000015008 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015008 |
long_lat |
ENVELOPE(-40.000,-40.000,-79.000,-79.000) ENVELOPE(27.000,27.000,-70.500,-70.500) |
geographic |
Antarctic The Antarctic Filchner Ice Shelf Prinsesse Ragnhild Kyst |
geographic_facet |
Antarctic The Antarctic Filchner Ice Shelf Prinsesse Ragnhild Kyst |
genre |
Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Journal of Glaciology Prinsesse Ragnhild Kyst |
genre_facet |
Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Journal of Glaciology Prinsesse Ragnhild Kyst |
op_source |
Journal of Glaciology volume 24, issue 90, page 484-485 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000015008 |
container_title |
Journal of Glaciology |
container_volume |
24 |
container_issue |
90 |
container_start_page |
484 |
op_container_end_page |
485 |
_version_ |
1792500140133580800 |