Should Glaciers Be Considered Permafrost?

This commentary critically evaluates concepts of extending the term permafrost to any parts of an active glacier. The whole mass of any glacier is at zero centigrade or below (cryotic), except for non-ice inclusions at the glacier surface. Therefore, if glacial ice is considered a monomineral rock,...

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Bibliographic Details
Published in:Geosciences
Main Author: Maciej Dąbski
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2019
Subjects:
Ice
Online Access:https://doi.org/10.3390/geosciences9120517
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spelling ftmdpi:oai:mdpi.com:/2076-3263/9/12/517/ 2023-08-20T04:07:06+02:00 Should Glaciers Be Considered Permafrost? Maciej Dąbski agris 2019-12-16 application/pdf https://doi.org/10.3390/geosciences9120517 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/geosciences9120517 https://creativecommons.org/licenses/by/4.0/ Geosciences; Volume 9; Issue 12; Pages: 517 glacial permafrost permafrost glacier–permafrost interactions polythermal glacier Text 2019 ftmdpi https://doi.org/10.3390/geosciences9120517 2023-07-31T22:54:18Z This commentary critically evaluates concepts of extending the term permafrost to any parts of an active glacier. The whole mass of any glacier is at zero centigrade or below (cryotic), except for non-ice inclusions at the glacier surface. Therefore, if glacial ice is considered a monomineral rock, then any glacier constitutes a perennially cryotic ground (i.e., permafrost), according to the purely thermal definition. However, extending the term permafrost to active glaciers introduces misconceptions, rather than a clarification of important geological terms. Text Ice permafrost MDPI Open Access Publishing Geosciences 9 12 517
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic glacial permafrost
permafrost
glacier–permafrost interactions
polythermal glacier
spellingShingle glacial permafrost
permafrost
glacier–permafrost interactions
polythermal glacier
Maciej Dąbski
Should Glaciers Be Considered Permafrost?
topic_facet glacial permafrost
permafrost
glacier–permafrost interactions
polythermal glacier
description This commentary critically evaluates concepts of extending the term permafrost to any parts of an active glacier. The whole mass of any glacier is at zero centigrade or below (cryotic), except for non-ice inclusions at the glacier surface. Therefore, if glacial ice is considered a monomineral rock, then any glacier constitutes a perennially cryotic ground (i.e., permafrost), according to the purely thermal definition. However, extending the term permafrost to active glaciers introduces misconceptions, rather than a clarification of important geological terms.
format Text
author Maciej Dąbski
author_facet Maciej Dąbski
author_sort Maciej Dąbski
title Should Glaciers Be Considered Permafrost?
title_short Should Glaciers Be Considered Permafrost?
title_full Should Glaciers Be Considered Permafrost?
title_fullStr Should Glaciers Be Considered Permafrost?
title_full_unstemmed Should Glaciers Be Considered Permafrost?
title_sort should glaciers be considered permafrost?
publisher Multidisciplinary Digital Publishing Institute
publishDate 2019
url https://doi.org/10.3390/geosciences9120517
op_coverage agris
genre Ice
permafrost
genre_facet Ice
permafrost
op_source Geosciences; Volume 9; Issue 12; Pages: 517
op_relation https://dx.doi.org/10.3390/geosciences9120517
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/geosciences9120517
container_title Geosciences
container_volume 9
container_issue 12
container_start_page 517
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