Study of Deformations within Ice Sheets due to Bottom Undulations by Means of Radio Echo-Sounding

Abstract In order to test the theory of glacier flow over bedrock undulations presented by S. J. Johnsen, K. Rasmussen, and N.Reeh in the accompanying abstract, data from the E.G.I.G. and the Dye-3 flow lines on the Greenland ice sheet have been analysed. The data comprise surface profiles measured...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Overgaard, S., Rasmussen, K.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1979
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000015203
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015203
_version_ 1821500561500930048
author Overgaard, S.
Rasmussen, K.
author_facet Overgaard, S.
Rasmussen, K.
author_sort Overgaard, S.
collection Cambridge University Press
container_issue 90
container_start_page 513
container_title Journal of Glaciology
container_volume 24
description Abstract In order to test the theory of glacier flow over bedrock undulations presented by S. J. Johnsen, K. Rasmussen, and N.Reeh in the accompanying abstract, data from the E.G.I.G. and the Dye-3 flow lines on the Greenland ice sheet have been analysed. The data comprise surface profiles measured by conventional techniques, and ice thicknesses and depths of internal isochronic layers obtained by the Technical University of Denmark by means of radio echo-soundings.
format Article in Journal/Newspaper
genre Dye 3
Dye-3
glacier
Greenland
Ice Sheet
Journal of Glaciology
genre_facet Dye 3
Dye-3
glacier
Greenland
Ice Sheet
Journal of Glaciology
geographic Greenland
Rasmussen
geographic_facet Greenland
Rasmussen
id crcambridgeupr:10.1017/s0022143000015203
institution Open Polar
language English
long_lat ENVELOPE(-64.084,-64.084,-65.248,-65.248)
op_collection_id crcambridgeupr
op_doi https://doi.org/10.1017/s0022143000015203
op_source Journal of Glaciology
volume 24, issue 90, page 513
ISSN 0022-1430 1727-5652
publishDate 1979
publisher Cambridge University Press (CUP)
record_format openpolar
spelling crcambridgeupr:10.1017/s0022143000015203 2025-01-16T21:40:21+00:00 Study of Deformations within Ice Sheets due to Bottom Undulations by Means of Radio Echo-Sounding Overgaard, S. Rasmussen, K. 1979 http://dx.doi.org/10.1017/s0022143000015203 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015203 en eng Cambridge University Press (CUP) Journal of Glaciology volume 24, issue 90, page 513 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1979 crcambridgeupr https://doi.org/10.1017/s0022143000015203 2024-02-08T08:37:11Z Abstract In order to test the theory of glacier flow over bedrock undulations presented by S. J. Johnsen, K. Rasmussen, and N.Reeh in the accompanying abstract, data from the E.G.I.G. and the Dye-3 flow lines on the Greenland ice sheet have been analysed. The data comprise surface profiles measured by conventional techniques, and ice thicknesses and depths of internal isochronic layers obtained by the Technical University of Denmark by means of radio echo-soundings. Article in Journal/Newspaper Dye 3 Dye-3 glacier Greenland Ice Sheet Journal of Glaciology Cambridge University Press Greenland Rasmussen ENVELOPE(-64.084,-64.084,-65.248,-65.248) Journal of Glaciology 24 90 513
spellingShingle Earth-Surface Processes
Overgaard, S.
Rasmussen, K.
Study of Deformations within Ice Sheets due to Bottom Undulations by Means of Radio Echo-Sounding
title Study of Deformations within Ice Sheets due to Bottom Undulations by Means of Radio Echo-Sounding
title_full Study of Deformations within Ice Sheets due to Bottom Undulations by Means of Radio Echo-Sounding
title_fullStr Study of Deformations within Ice Sheets due to Bottom Undulations by Means of Radio Echo-Sounding
title_full_unstemmed Study of Deformations within Ice Sheets due to Bottom Undulations by Means of Radio Echo-Sounding
title_short Study of Deformations within Ice Sheets due to Bottom Undulations by Means of Radio Echo-Sounding
title_sort study of deformations within ice sheets due to bottom undulations by means of radio echo-sounding
topic Earth-Surface Processes
topic_facet Earth-Surface Processes
url http://dx.doi.org/10.1017/s0022143000015203
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015203