Diagnostics and Mapping of Geoecological Situations in the Permafrost Zone of Russia

The diagnosis of the geoecological state of natural landscapes during the economic development of the permafrost zone should be established by assessing destructive cryogenic processes. Furthermore, the geoecological state should be considered in terms of landscape resistance to an increase in cryog...

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Published in:Geosciences
Main Authors: Nellie Tumel, Larisa Zotova
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2019
Subjects:
Ice
Online Access:https://doi.org/10.3390/geosciences9080353
https://doaj.org/article/e68a4653b56d49ef82aa9ed4749509a4
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spelling ftdoajarticles:oai:doaj.org/article:e68a4653b56d49ef82aa9ed4749509a4 2023-05-15T16:37:18+02:00 Diagnostics and Mapping of Geoecological Situations in the Permafrost Zone of Russia Nellie Tumel Larisa Zotova 2019-08-01T00:00:00Z https://doi.org/10.3390/geosciences9080353 https://doaj.org/article/e68a4653b56d49ef82aa9ed4749509a4 EN eng MDPI AG https://www.mdpi.com/2076-3263/9/8/353 https://doaj.org/toc/2076-3263 2076-3263 doi:10.3390/geosciences9080353 https://doaj.org/article/e68a4653b56d49ef82aa9ed4749509a4 Geosciences, Vol 9, Iss 8, p 353 (2019) geoecological situations permafrost zone cryolithozone cryogenic processes landscapes stability expert assessments geoinformation mapping Geology QE1-996.5 article 2019 ftdoajarticles https://doi.org/10.3390/geosciences9080353 2022-12-31T05:56:38Z The diagnosis of the geoecological state of natural landscapes during the economic development of the permafrost zone should be established by assessing destructive cryogenic processes. Furthermore, the geoecological state should be considered in terms of landscape resistance to an increase in cryogenic processes. In this paper, we examine and determine lithocryogenic stability parameters, including permafrost distribution over an area, annual mean temperature, ice content (humidity), and the protective properties of the vegetation. Activation of cryogenic processes in Western Siberia was estimated in terms of the area, development rate and attenuation, natural landscape damage, and hazards to engineering and mining facility operations. The evaluation procedure and the improvement in expert numerical scores are shown. A number of approved methods are proposed for creating assessment maps at various scales using landscape indication methods, decoded satellite images, expert assessments, statistical calculations, and analysis of spatial geographical information systems. Methodical techniques for digital geocryological mapping on the basis of the landscape are presented at scales from 1:3,000,000 to 1:20,000,000. All the maps were created by the authors and can be used for a wide range of applications, including design, survey organizations, and education. Article in Journal/Newspaper Ice permafrost Siberia Directory of Open Access Journals: DOAJ Articles Geosciences 9 8 353
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic geoecological situations
permafrost zone
cryolithozone
cryogenic processes
landscapes stability
expert assessments
geoinformation mapping
Geology
QE1-996.5
spellingShingle geoecological situations
permafrost zone
cryolithozone
cryogenic processes
landscapes stability
expert assessments
geoinformation mapping
Geology
QE1-996.5
Nellie Tumel
Larisa Zotova
Diagnostics and Mapping of Geoecological Situations in the Permafrost Zone of Russia
topic_facet geoecological situations
permafrost zone
cryolithozone
cryogenic processes
landscapes stability
expert assessments
geoinformation mapping
Geology
QE1-996.5
description The diagnosis of the geoecological state of natural landscapes during the economic development of the permafrost zone should be established by assessing destructive cryogenic processes. Furthermore, the geoecological state should be considered in terms of landscape resistance to an increase in cryogenic processes. In this paper, we examine and determine lithocryogenic stability parameters, including permafrost distribution over an area, annual mean temperature, ice content (humidity), and the protective properties of the vegetation. Activation of cryogenic processes in Western Siberia was estimated in terms of the area, development rate and attenuation, natural landscape damage, and hazards to engineering and mining facility operations. The evaluation procedure and the improvement in expert numerical scores are shown. A number of approved methods are proposed for creating assessment maps at various scales using landscape indication methods, decoded satellite images, expert assessments, statistical calculations, and analysis of spatial geographical information systems. Methodical techniques for digital geocryological mapping on the basis of the landscape are presented at scales from 1:3,000,000 to 1:20,000,000. All the maps were created by the authors and can be used for a wide range of applications, including design, survey organizations, and education.
format Article in Journal/Newspaper
author Nellie Tumel
Larisa Zotova
author_facet Nellie Tumel
Larisa Zotova
author_sort Nellie Tumel
title Diagnostics and Mapping of Geoecological Situations in the Permafrost Zone of Russia
title_short Diagnostics and Mapping of Geoecological Situations in the Permafrost Zone of Russia
title_full Diagnostics and Mapping of Geoecological Situations in the Permafrost Zone of Russia
title_fullStr Diagnostics and Mapping of Geoecological Situations in the Permafrost Zone of Russia
title_full_unstemmed Diagnostics and Mapping of Geoecological Situations in the Permafrost Zone of Russia
title_sort diagnostics and mapping of geoecological situations in the permafrost zone of russia
publisher MDPI AG
publishDate 2019
url https://doi.org/10.3390/geosciences9080353
https://doaj.org/article/e68a4653b56d49ef82aa9ed4749509a4
genre Ice
permafrost
Siberia
genre_facet Ice
permafrost
Siberia
op_source Geosciences, Vol 9, Iss 8, p 353 (2019)
op_relation https://www.mdpi.com/2076-3263/9/8/353
https://doaj.org/toc/2076-3263
2076-3263
doi:10.3390/geosciences9080353
https://doaj.org/article/e68a4653b56d49ef82aa9ed4749509a4
op_doi https://doi.org/10.3390/geosciences9080353
container_title Geosciences
container_volume 9
container_issue 8
container_start_page 353
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