Contribution to the Knowledge of the Antarctic Ice Sheet: A Synthesis of Glaciological Measurements in Terre Adélie

Abstract This paper is a synthesis of glaciological investigations conducted in Terre Adélie, mainly during the LG.Y. The surface and bedrock profiles have been obtained along a 500 km. line roughly perpendicular to the coast; the mean annual temperature has been studied as a finnction of altitude,...

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Published in:Journal of Glaciology
Main Author: Lorius, C.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1962
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000018220
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000018220
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spelling crcambridgeupr:10.1017/s0022143000018220 2024-03-03T08:38:47+00:00 Contribution to the Knowledge of the Antarctic Ice Sheet: A Synthesis of Glaciological Measurements in Terre Adélie Lorius, C. 1962 http://dx.doi.org/10.1017/s0022143000018220 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000018220 en eng Cambridge University Press (CUP) Journal of Glaciology volume 4, issue 31, page 79-92 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1962 crcambridgeupr https://doi.org/10.1017/s0022143000018220 2024-02-08T08:47:47Z Abstract This paper is a synthesis of glaciological investigations conducted in Terre Adélie, mainly during the LG.Y. The surface and bedrock profiles have been obtained along a 500 km. line roughly perpendicular to the coast; the mean annual temperature has been studied as a finnction of altitude, and mean accumulation has been related to distance from the coast and surface slope. Stratigraphic studies made at Station Charcot again raise the problem of the determination of mean accumulation in certain parts of the Antarctic plateau; they provide a quadratic relationship between density and depth. The snow-drift studies lead to the Mowing conclusions: wind velocity and density of drifting snow are functions of height above the surface, and the total transport depends on wind velocity. Lastly, measurements have been made of glacier flow near the coast. The paper ends with a schematic study of the mass balance in Terre Adélie; accumulation seems to be slightly larger than ablation, a result that is to be contrasted with the obtervrd coastal retreat near Dumont d’Urille base. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Journal of Glaciology Cambridge University Press Antarctic The Antarctic Terre Adélie ENVELOPE(139.000,139.000,-67.000,-67.000) Terre-Adélie ENVELOPE(138.991,138.991,-59.999,-59.999) Charcot ENVELOPE(139.017,139.017,-69.367,-69.367) Station Charcot ENVELOPE(139.017,139.017,-69.367,-69.367) Journal of Glaciology 4 31 79 92
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Lorius, C.
Contribution to the Knowledge of the Antarctic Ice Sheet: A Synthesis of Glaciological Measurements in Terre Adélie
topic_facet Earth-Surface Processes
description Abstract This paper is a synthesis of glaciological investigations conducted in Terre Adélie, mainly during the LG.Y. The surface and bedrock profiles have been obtained along a 500 km. line roughly perpendicular to the coast; the mean annual temperature has been studied as a finnction of altitude, and mean accumulation has been related to distance from the coast and surface slope. Stratigraphic studies made at Station Charcot again raise the problem of the determination of mean accumulation in certain parts of the Antarctic plateau; they provide a quadratic relationship between density and depth. The snow-drift studies lead to the Mowing conclusions: wind velocity and density of drifting snow are functions of height above the surface, and the total transport depends on wind velocity. Lastly, measurements have been made of glacier flow near the coast. The paper ends with a schematic study of the mass balance in Terre Adélie; accumulation seems to be slightly larger than ablation, a result that is to be contrasted with the obtervrd coastal retreat near Dumont d’Urille base.
format Article in Journal/Newspaper
author Lorius, C.
author_facet Lorius, C.
author_sort Lorius, C.
title Contribution to the Knowledge of the Antarctic Ice Sheet: A Synthesis of Glaciological Measurements in Terre Adélie
title_short Contribution to the Knowledge of the Antarctic Ice Sheet: A Synthesis of Glaciological Measurements in Terre Adélie
title_full Contribution to the Knowledge of the Antarctic Ice Sheet: A Synthesis of Glaciological Measurements in Terre Adélie
title_fullStr Contribution to the Knowledge of the Antarctic Ice Sheet: A Synthesis of Glaciological Measurements in Terre Adélie
title_full_unstemmed Contribution to the Knowledge of the Antarctic Ice Sheet: A Synthesis of Glaciological Measurements in Terre Adélie
title_sort contribution to the knowledge of the antarctic ice sheet: a synthesis of glaciological measurements in terre adélie
publisher Cambridge University Press (CUP)
publishDate 1962
url http://dx.doi.org/10.1017/s0022143000018220
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000018220
long_lat ENVELOPE(139.000,139.000,-67.000,-67.000)
ENVELOPE(138.991,138.991,-59.999,-59.999)
ENVELOPE(139.017,139.017,-69.367,-69.367)
ENVELOPE(139.017,139.017,-69.367,-69.367)
geographic Antarctic
The Antarctic
Terre Adélie
Terre-Adélie
Charcot
Station Charcot
geographic_facet Antarctic
The Antarctic
Terre Adélie
Terre-Adélie
Charcot
Station Charcot
genre Antarc*
Antarctic
Ice Sheet
Journal of Glaciology
genre_facet Antarc*
Antarctic
Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology
volume 4, issue 31, page 79-92
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000018220
container_title Journal of Glaciology
container_volume 4
container_issue 31
container_start_page 79
op_container_end_page 92
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