Distribution and Character of Naleds in Northeastern Alaska

Satellite imagery and high- and low-altitude aerial photography of the North Slope of Alaska indicate that naleds (features formed during river icing) are widespread east of the Colville River but less abundant to its west. Where naleds occur, stream channels are wide and often braided. Their distri...

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Bibliographic Details
Published in:ARCTIC
Main Authors: Harden, Deborah, Barnes, Peter, Reimnitz, Erk
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1977
Subjects:
Ice
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65733
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/65733 2023-05-15T14:19:18+02:00 Distribution and Character of Naleds in Northeastern Alaska Harden, Deborah Barnes, Peter Reimnitz, Erk 1977-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65733 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65733/49647 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65733 ARCTIC; Vol. 30 No. 1 (1977): March: 1–68; 28-40 1923-1245 0004-0843 Formation River ice Alaska Northern Kongakut River info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1977 ftunivcalgaryojs 2022-03-22T21:22:45Z Satellite imagery and high- and low-altitude aerial photography of the North Slope of Alaska indicate that naleds (features formed during river icing) are widespread east of the Colville River but less abundant to its west. Where naleds occur, stream channels are wide and often braided. Their distribution can be related to changes in stream gradient and to the occurrence of springs. Large naleds, such as occur on the Kongakut River, often survive the summer melt season to form the nucleus of icing in the succeeding winter. Major naleds also are likely to significantly influence the nature of permafrost in their immediate vicinity. A map of naleds may serve as a guide to sources of perennially flowing water. Article in Journal/Newspaper Arctic Ice north slope permafrost Alaska University of Calgary Journal Hosting ARCTIC 30 1
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Formation
River ice
Alaska
Northern
Kongakut River
spellingShingle Formation
River ice
Alaska
Northern
Kongakut River
Harden, Deborah
Barnes, Peter
Reimnitz, Erk
Distribution and Character of Naleds in Northeastern Alaska
topic_facet Formation
River ice
Alaska
Northern
Kongakut River
description Satellite imagery and high- and low-altitude aerial photography of the North Slope of Alaska indicate that naleds (features formed during river icing) are widespread east of the Colville River but less abundant to its west. Where naleds occur, stream channels are wide and often braided. Their distribution can be related to changes in stream gradient and to the occurrence of springs. Large naleds, such as occur on the Kongakut River, often survive the summer melt season to form the nucleus of icing in the succeeding winter. Major naleds also are likely to significantly influence the nature of permafrost in their immediate vicinity. A map of naleds may serve as a guide to sources of perennially flowing water.
format Article in Journal/Newspaper
author Harden, Deborah
Barnes, Peter
Reimnitz, Erk
author_facet Harden, Deborah
Barnes, Peter
Reimnitz, Erk
author_sort Harden, Deborah
title Distribution and Character of Naleds in Northeastern Alaska
title_short Distribution and Character of Naleds in Northeastern Alaska
title_full Distribution and Character of Naleds in Northeastern Alaska
title_fullStr Distribution and Character of Naleds in Northeastern Alaska
title_full_unstemmed Distribution and Character of Naleds in Northeastern Alaska
title_sort distribution and character of naleds in northeastern alaska
publisher The Arctic Institute of North America
publishDate 1977
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65733
genre Arctic
Ice
north slope
permafrost
Alaska
genre_facet Arctic
Ice
north slope
permafrost
Alaska
op_source ARCTIC; Vol. 30 No. 1 (1977): March: 1–68; 28-40
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65733/49647
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65733
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