Fifty years of progress in understanding ice sheets

Over the past 50 years, ideas relating to the physical features and dynamics of ice sheets have evolved materially, primarily due to modern technological advances in the acquisition of basic data. This paper therefore does not review contemporary knowledge but records how our perception of ice sheet...

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Published in:Journal of Glaciology
Main Authors: Robin, Gordon de Q., Swithinbank, Charles
Format: Article in Journal/Newspaper
Language:unknown
Published: International Glaciological Society 1987
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/522945/
https://doi.org/10.3189/S0022143000215803
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spelling ftnerc:oai:nora.nerc.ac.uk:522945 2023-05-15T13:41:43+02:00 Fifty years of progress in understanding ice sheets Robin, Gordon de Q. Swithinbank, Charles 1987 http://nora.nerc.ac.uk/id/eprint/522945/ https://doi.org/10.3189/S0022143000215803 unknown International Glaciological Society Robin, Gordon de Q.; Swithinbank, Charles. 1987 Fifty years of progress in understanding ice sheets. Journal of Glaciology, 33 (S1). 33-47. https://doi.org/10.3189/S0022143000215803 <https://doi.org/10.3189/S0022143000215803> Publication - Article PeerReviewed 1987 ftnerc https://doi.org/10.3189/S0022143000215803 2023-02-04T19:48:08Z Over the past 50 years, ideas relating to the physical features and dynamics of ice sheets have evolved materially, primarily due to modern technological advances in the acquisition of basic data. This paper therefore does not review contemporary knowledge but records how our perception of ice sheets has changed with time. Rather than dealing with individual contributions to the understanding of ice sheets, major topics and concepts are considered against a background of earlier ideas and theories. Both the form and extent of the surface features of ice sheets have been defined more clearly by the relatively recent use of satellite studies (imagery and altimetry). In an analogous way, radio echo-sounding has enabled the accurate calculation of ice thicknesses and the mapping of the sub-ice bedrock contours, and hence estimation of the ice volume. Studies on the dynamics of ice sheets have been enhanced by bore-hole sampling of deep ice and the determination of ice-temperature distributions, coupled with measurements of mass balance and both surface and internal ice movement. Internal deformation of ice sheets, surging, and various flow theories are considered in relation to recent modelling studies. Global geophysics inevitably includes the role of ice sheets, and therefore climatological studies and new atmospheric chemistry data, together with information on the distribution of meteorites on the Antarctic ice sheet, are considered critically. Modern concepts of the evolution of ice sheets have substantially modified earlier ideas of the glacial geologists and have explained much that had previously mystified them. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Journal of Glaciology Natural Environment Research Council: NERC Open Research Archive Antarctic The Antarctic Journal of Glaciology 33 S1 33 47
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
description Over the past 50 years, ideas relating to the physical features and dynamics of ice sheets have evolved materially, primarily due to modern technological advances in the acquisition of basic data. This paper therefore does not review contemporary knowledge but records how our perception of ice sheets has changed with time. Rather than dealing with individual contributions to the understanding of ice sheets, major topics and concepts are considered against a background of earlier ideas and theories. Both the form and extent of the surface features of ice sheets have been defined more clearly by the relatively recent use of satellite studies (imagery and altimetry). In an analogous way, radio echo-sounding has enabled the accurate calculation of ice thicknesses and the mapping of the sub-ice bedrock contours, and hence estimation of the ice volume. Studies on the dynamics of ice sheets have been enhanced by bore-hole sampling of deep ice and the determination of ice-temperature distributions, coupled with measurements of mass balance and both surface and internal ice movement. Internal deformation of ice sheets, surging, and various flow theories are considered in relation to recent modelling studies. Global geophysics inevitably includes the role of ice sheets, and therefore climatological studies and new atmospheric chemistry data, together with information on the distribution of meteorites on the Antarctic ice sheet, are considered critically. Modern concepts of the evolution of ice sheets have substantially modified earlier ideas of the glacial geologists and have explained much that had previously mystified them.
format Article in Journal/Newspaper
author Robin, Gordon de Q.
Swithinbank, Charles
spellingShingle Robin, Gordon de Q.
Swithinbank, Charles
Fifty years of progress in understanding ice sheets
author_facet Robin, Gordon de Q.
Swithinbank, Charles
author_sort Robin, Gordon de Q.
title Fifty years of progress in understanding ice sheets
title_short Fifty years of progress in understanding ice sheets
title_full Fifty years of progress in understanding ice sheets
title_fullStr Fifty years of progress in understanding ice sheets
title_full_unstemmed Fifty years of progress in understanding ice sheets
title_sort fifty years of progress in understanding ice sheets
publisher International Glaciological Society
publishDate 1987
url http://nora.nerc.ac.uk/id/eprint/522945/
https://doi.org/10.3189/S0022143000215803
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Ice Sheet
Journal of Glaciology
genre_facet Antarc*
Antarctic
Ice Sheet
Journal of Glaciology
op_relation Robin, Gordon de Q.; Swithinbank, Charles. 1987 Fifty years of progress in understanding ice sheets. Journal of Glaciology, 33 (S1). 33-47. https://doi.org/10.3189/S0022143000215803 <https://doi.org/10.3189/S0022143000215803>
op_doi https://doi.org/10.3189/S0022143000215803
container_title Journal of Glaciology
container_volume 33
container_issue S1
container_start_page 33
op_container_end_page 47
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