Cryoconite Holes on Sermikavsak, West Greenland

Abstract The depths and diameters of 158 cryoconite holes were measured at ten positions in the ablation zone of Sermikavsak, West Greenland. It was found that the depths increased on going up the glacier in agreement with other measurements made earlier on polar glaciers. There was no significant c...

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Published in:Journal of Glaciology
Main Author: Gribbon, P. W. F.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1979
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000014167
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014167
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spelling crcambridgeupr:10.1017/s0022143000014167 2024-06-16T07:40:08+00:00 Cryoconite Holes on Sermikavsak, West Greenland Gribbon, P. W. F. 1979 http://dx.doi.org/10.1017/s0022143000014167 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014167 en eng Cambridge University Press (CUP) Journal of Glaciology volume 22, issue 86, page 177-181 ISSN 0022-1430 1727-5652 journal-article 1979 crcambridgeupr https://doi.org/10.1017/s0022143000014167 2024-05-22T12:56:35Z Abstract The depths and diameters of 158 cryoconite holes were measured at ten positions in the ablation zone of Sermikavsak, West Greenland. It was found that the depths increased on going up the glacier in agreement with other measurements made earlier on polar glaciers. There was no significant correlation of depth with diameter. The relative importance of the combined short- and long-wavelength radiation balances and the transfer of heat by convectional mixing in water-filled holes is discussed. The variations in depth are attributed to changes in the albedo and the bulk extinction coefficient of the surface ice layers on the glacier. Article in Journal/Newspaper glacier Greenland Journal of Glaciology Cambridge University Press Greenland Sermikavsak ENVELOPE(-51.700,-51.700,71.033,71.033) Journal of Glaciology 22 86 177 181
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract The depths and diameters of 158 cryoconite holes were measured at ten positions in the ablation zone of Sermikavsak, West Greenland. It was found that the depths increased on going up the glacier in agreement with other measurements made earlier on polar glaciers. There was no significant correlation of depth with diameter. The relative importance of the combined short- and long-wavelength radiation balances and the transfer of heat by convectional mixing in water-filled holes is discussed. The variations in depth are attributed to changes in the albedo and the bulk extinction coefficient of the surface ice layers on the glacier.
format Article in Journal/Newspaper
author Gribbon, P. W. F.
spellingShingle Gribbon, P. W. F.
Cryoconite Holes on Sermikavsak, West Greenland
author_facet Gribbon, P. W. F.
author_sort Gribbon, P. W. F.
title Cryoconite Holes on Sermikavsak, West Greenland
title_short Cryoconite Holes on Sermikavsak, West Greenland
title_full Cryoconite Holes on Sermikavsak, West Greenland
title_fullStr Cryoconite Holes on Sermikavsak, West Greenland
title_full_unstemmed Cryoconite Holes on Sermikavsak, West Greenland
title_sort cryoconite holes on sermikavsak, west greenland
publisher Cambridge University Press (CUP)
publishDate 1979
url http://dx.doi.org/10.1017/s0022143000014167
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014167
long_lat ENVELOPE(-51.700,-51.700,71.033,71.033)
geographic Greenland
Sermikavsak
geographic_facet Greenland
Sermikavsak
genre glacier
Greenland
Journal of Glaciology
genre_facet glacier
Greenland
Journal of Glaciology
op_source Journal of Glaciology
volume 22, issue 86, page 177-181
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000014167
container_title Journal of Glaciology
container_volume 22
container_issue 86
container_start_page 177
op_container_end_page 181
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