A Mathematical Model for Perched Block Formation

Abstract A mathematical model for the formation of perched blocks on glaciers due to differential ablation is developed by considering energy balances. The model is applied to naturally positioned rocks on Bersærkerbræ, Greenland. The model predicts correctly whether a rock will perch or sink in ele...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Patterson, E. A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1984
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000006122
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006122
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spelling crcambridgeupr:10.1017/s0022143000006122 2023-06-11T04:11:55+02:00 A Mathematical Model for Perched Block Formation Patterson, E. A. 1984 http://dx.doi.org/10.1017/s0022143000006122 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006122 en eng Cambridge University Press (CUP) Journal of Glaciology volume 30, issue 106, page 296-301 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1984 crcambridgeupr https://doi.org/10.1017/s0022143000006122 2023-05-01T18:21:02Z Abstract A mathematical model for the formation of perched blocks on glaciers due to differential ablation is developed by considering energy balances. The model is applied to naturally positioned rocks on Bersærkerbræ, Greenland. The model predicts correctly whether a rock will perch or sink in eleven out of twelve cases. For artificially positioned small rocks of mean dimension 0.2 m, the model has a 53% success rate. The reduced performance is probably due to the thicknesses of the rocks being of similar magnitude to the range of relief of the glacier surface. Article in Journal/Newspaper glacier Greenland Journal of Glaciology Cambridge University Press (via Crossref) Bersærkerbræ ENVELOPE(-24.617,-24.617,72.133,72.133) Greenland Journal of Glaciology 30 106 296 301
institution Open Polar
collection Cambridge University Press (via Crossref)
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Patterson, E. A.
A Mathematical Model for Perched Block Formation
topic_facet Earth-Surface Processes
description Abstract A mathematical model for the formation of perched blocks on glaciers due to differential ablation is developed by considering energy balances. The model is applied to naturally positioned rocks on Bersærkerbræ, Greenland. The model predicts correctly whether a rock will perch or sink in eleven out of twelve cases. For artificially positioned small rocks of mean dimension 0.2 m, the model has a 53% success rate. The reduced performance is probably due to the thicknesses of the rocks being of similar magnitude to the range of relief of the glacier surface.
format Article in Journal/Newspaper
author Patterson, E. A.
author_facet Patterson, E. A.
author_sort Patterson, E. A.
title A Mathematical Model for Perched Block Formation
title_short A Mathematical Model for Perched Block Formation
title_full A Mathematical Model for Perched Block Formation
title_fullStr A Mathematical Model for Perched Block Formation
title_full_unstemmed A Mathematical Model for Perched Block Formation
title_sort mathematical model for perched block formation
publisher Cambridge University Press (CUP)
publishDate 1984
url http://dx.doi.org/10.1017/s0022143000006122
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006122
long_lat ENVELOPE(-24.617,-24.617,72.133,72.133)
geographic Bersærkerbræ
Greenland
geographic_facet Bersærkerbræ
Greenland
genre glacier
Greenland
Journal of Glaciology
genre_facet glacier
Greenland
Journal of Glaciology
op_source Journal of Glaciology
volume 30, issue 106, page 296-301
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000006122
container_title Journal of Glaciology
container_volume 30
container_issue 106
container_start_page 296
op_container_end_page 301
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