Flow of the Brunt Ice Shelf, Antarctica, derived from Landsat images, 1974–85
Satellite images recorded in 1973, 1974, and 1985 of the Brunt Ice Shelf are compared. There are sufficient identifiable features moving with the ice shelf to show flow patterns over an area of ~10 000 km2. Velocities vary from 500 m a−1 in the west, near the Dawson-Lambton Ice Stream, to 1300 m a−1...
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International Glaciological Society
1986
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Online Access: | http://nora.nerc.ac.uk/id/eprint/523169/ https://doi.org/10.3189/S0022143000015586 |
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ftnerc:oai:nora.nerc.ac.uk:523169 2023-05-15T13:41:43+02:00 Flow of the Brunt Ice Shelf, Antarctica, derived from Landsat images, 1974–85 Simmons, D.A. 1986 http://nora.nerc.ac.uk/id/eprint/523169/ https://doi.org/10.3189/S0022143000015586 unknown International Glaciological Society Simmons, D.A. 1986 Flow of the Brunt Ice Shelf, Antarctica, derived from Landsat images, 1974–85. Journal of Glaciology, 32 (111). 252-254. https://doi.org/10.3189/S0022143000015586 <https://doi.org/10.3189/S0022143000015586> Publication - Article PeerReviewed 1986 ftnerc https://doi.org/10.3189/S0022143000015586 2023-02-04T19:48:15Z Satellite images recorded in 1973, 1974, and 1985 of the Brunt Ice Shelf are compared. There are sufficient identifiable features moving with the ice shelf to show flow patterns over an area of ~10 000 km2. Velocities vary from 500 m a−1 in the west, near the Dawson-Lambton Ice Stream, to 1300 m a−1 in the east, within the Stancomb-Wills Ice Stream. Article in Journal/Newspaper Antarc* Antarctica Brunt Ice Shelf Ice Shelf Journal of Glaciology Natural Environment Research Council: NERC Open Research Archive Brunt Ice Shelf ENVELOPE(-22.500,-22.500,-74.750,-74.750) Stancomb-Wills Ice Stream ENVELOPE(-20.000,-20.000,-75.300,-75.300) Dawson-Lambton ENVELOPE(160.617,160.617,-78.900,-78.900) Dawson-Lambton Ice Stream ENVELOPE(-26.000,-26.000,-76.500,-76.500) Journal of Glaciology 32 111 252 254 |
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Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
unknown |
description |
Satellite images recorded in 1973, 1974, and 1985 of the Brunt Ice Shelf are compared. There are sufficient identifiable features moving with the ice shelf to show flow patterns over an area of ~10 000 km2. Velocities vary from 500 m a−1 in the west, near the Dawson-Lambton Ice Stream, to 1300 m a−1 in the east, within the Stancomb-Wills Ice Stream. |
format |
Article in Journal/Newspaper |
author |
Simmons, D.A. |
spellingShingle |
Simmons, D.A. Flow of the Brunt Ice Shelf, Antarctica, derived from Landsat images, 1974–85 |
author_facet |
Simmons, D.A. |
author_sort |
Simmons, D.A. |
title |
Flow of the Brunt Ice Shelf, Antarctica, derived from Landsat images, 1974–85 |
title_short |
Flow of the Brunt Ice Shelf, Antarctica, derived from Landsat images, 1974–85 |
title_full |
Flow of the Brunt Ice Shelf, Antarctica, derived from Landsat images, 1974–85 |
title_fullStr |
Flow of the Brunt Ice Shelf, Antarctica, derived from Landsat images, 1974–85 |
title_full_unstemmed |
Flow of the Brunt Ice Shelf, Antarctica, derived from Landsat images, 1974–85 |
title_sort |
flow of the brunt ice shelf, antarctica, derived from landsat images, 1974–85 |
publisher |
International Glaciological Society |
publishDate |
1986 |
url |
http://nora.nerc.ac.uk/id/eprint/523169/ https://doi.org/10.3189/S0022143000015586 |
long_lat |
ENVELOPE(-22.500,-22.500,-74.750,-74.750) ENVELOPE(-20.000,-20.000,-75.300,-75.300) ENVELOPE(160.617,160.617,-78.900,-78.900) ENVELOPE(-26.000,-26.000,-76.500,-76.500) |
geographic |
Brunt Ice Shelf Stancomb-Wills Ice Stream Dawson-Lambton Dawson-Lambton Ice Stream |
geographic_facet |
Brunt Ice Shelf Stancomb-Wills Ice Stream Dawson-Lambton Dawson-Lambton Ice Stream |
genre |
Antarc* Antarctica Brunt Ice Shelf Ice Shelf Journal of Glaciology |
genre_facet |
Antarc* Antarctica Brunt Ice Shelf Ice Shelf Journal of Glaciology |
op_relation |
Simmons, D.A. 1986 Flow of the Brunt Ice Shelf, Antarctica, derived from Landsat images, 1974–85. Journal of Glaciology, 32 (111). 252-254. https://doi.org/10.3189/S0022143000015586 <https://doi.org/10.3189/S0022143000015586> |
op_doi |
https://doi.org/10.3189/S0022143000015586 |
container_title |
Journal of Glaciology |
container_volume |
32 |
container_issue |
111 |
container_start_page |
252 |
op_container_end_page |
254 |
_version_ |
1766154775631495168 |