Flow of the Brunt Ice Shelf, Antarctica, Derived from Landsat Images, 1974–85

Abstract 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 km 2 . Velocities vary from 500 m a −1 in the west, near the Dawson-Lambton Ice Stream, t...

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Published in:Journal of Glaciology
Main Author: Simmons, D.A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1986
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000015586
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015586
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spelling crcambridgeupr:10.1017/s0022143000015586 2024-03-03T08:38:02+00:00 Flow of the Brunt Ice Shelf, Antarctica, Derived from Landsat Images, 1974–85 Simmons, D.A. 1986 http://dx.doi.org/10.1017/s0022143000015586 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015586 en eng Cambridge University Press (CUP) Journal of Glaciology volume 32, issue 111, page 252-254 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1986 crcambridgeupr https://doi.org/10.1017/s0022143000015586 2024-02-08T08:34:04Z Abstract 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 km 2 . 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 Cambridge University Press 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
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Simmons, D.A.
Flow of the Brunt Ice Shelf, Antarctica, Derived from Landsat Images, 1974–85
topic_facet Earth-Surface Processes
description Abstract 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 km 2 . 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.
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 Cambridge University Press (CUP)
publishDate 1986
url http://dx.doi.org/10.1017/s0022143000015586
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/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_source Journal of Glaciology
volume 32, issue 111, page 252-254
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000015586
container_title Journal of Glaciology
container_volume 32
container_issue 111
container_start_page 252
op_container_end_page 254
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