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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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Simmons, D.A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1986
Subjects:
Earth-Surface Processes
Brunt Ice Shelf
Stancomb-Wills Ice Stream
Dawson-Lambton
Dawson-Lambton Ice Stream
Antarc*
Antarctica
Ice Shelf
Journal of Glaciology
Online Access:http://dx.doi.org/10.1017/s0022143000015586
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015586
Description
Summary: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.

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