Post-Surge Temperatures in Steele Glacier, Yukon Territory, Canada

Abstract Deep ice temperatures measured at four widely spaced sites on Steele Glacier show that the thermal regime was profoundly influenced by the 1965-66 surge advance. Three of four measured temperature profiles are "anomalous" in that the upper 100 m of ice is far from thermal equilibr...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Clarke, Garry K.C., Jarvis, Gary T.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1976
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000031580
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031580
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spelling crcambridgeupr:10.1017/s0022143000031580 2024-03-03T08:44:40+00:00 Post-Surge Temperatures in Steele Glacier, Yukon Territory, Canada Clarke, Garry K.C. Jarvis, Gary T. 1976 http://dx.doi.org/10.1017/s0022143000031580 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031580 en eng Cambridge University Press (CUP) Journal of Glaciology volume 16, issue 74, page 261-268 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1976 crcambridgeupr https://doi.org/10.1017/s0022143000031580 2024-02-08T08:42:50Z Abstract Deep ice temperatures measured at four widely spaced sites on Steele Glacier show that the thermal regime was profoundly influenced by the 1965-66 surge advance. Three of four measured temperature profiles are "anomalous" in that the upper 100 m of ice is far from thermal equilibrium. Water penetration during the surge is the probable cause of these anomalies. Insufficient data are available to predict the basal ice temperature. Article in Journal/Newspaper glacier* Journal of Glaciology Yukon Cambridge University Press Yukon Canada Steele ENVELOPE(-60.710,-60.710,-70.980,-70.980) Steele Glacier ENVELOPE(-140.171,-140.171,61.249,61.249) Journal of Glaciology 16 74 261 268
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Clarke, Garry K.C.
Jarvis, Gary T.
Post-Surge Temperatures in Steele Glacier, Yukon Territory, Canada
topic_facet Earth-Surface Processes
description Abstract Deep ice temperatures measured at four widely spaced sites on Steele Glacier show that the thermal regime was profoundly influenced by the 1965-66 surge advance. Three of four measured temperature profiles are "anomalous" in that the upper 100 m of ice is far from thermal equilibrium. Water penetration during the surge is the probable cause of these anomalies. Insufficient data are available to predict the basal ice temperature.
format Article in Journal/Newspaper
author Clarke, Garry K.C.
Jarvis, Gary T.
author_facet Clarke, Garry K.C.
Jarvis, Gary T.
author_sort Clarke, Garry K.C.
title Post-Surge Temperatures in Steele Glacier, Yukon Territory, Canada
title_short Post-Surge Temperatures in Steele Glacier, Yukon Territory, Canada
title_full Post-Surge Temperatures in Steele Glacier, Yukon Territory, Canada
title_fullStr Post-Surge Temperatures in Steele Glacier, Yukon Territory, Canada
title_full_unstemmed Post-Surge Temperatures in Steele Glacier, Yukon Territory, Canada
title_sort post-surge temperatures in steele glacier, yukon territory, canada
publisher Cambridge University Press (CUP)
publishDate 1976
url http://dx.doi.org/10.1017/s0022143000031580
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031580
long_lat ENVELOPE(-60.710,-60.710,-70.980,-70.980)
ENVELOPE(-140.171,-140.171,61.249,61.249)
geographic Yukon
Canada
Steele
Steele Glacier
geographic_facet Yukon
Canada
Steele
Steele Glacier
genre glacier*
Journal of Glaciology
Yukon
genre_facet glacier*
Journal of Glaciology
Yukon
op_source Journal of Glaciology
volume 16, issue 74, page 261-268
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000031580
container_title Journal of Glaciology
container_volume 16
container_issue 74
container_start_page 261
op_container_end_page 268
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