Advantages of the basin approach for investigations of aufeises (naleds)
Formation of aufeises (naleds) is rather widely distributed cryogenic process in the permafrost zone, therefore naleds are reasonably called the seasonal glaciation of the planet. The ever-increasing interest in aufeises significantly extends the thematic focus of studying them. Various methodologic...
Published in: | Ice and Snow |
---|---|
Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | Russian |
Published: |
Nauka
2016
|
Subjects: | |
Online Access: | https://doi.org/10.15356/2076-6734-2016-3-381-386 https://doaj.org/article/90cd9d74cdaf4ce895e3045fdb8012f0 |
id |
ftdoajarticles:oai:doaj.org/article:90cd9d74cdaf4ce895e3045fdb8012f0 |
---|---|
record_format |
openpolar |
spelling |
ftdoajarticles:oai:doaj.org/article:90cd9d74cdaf4ce895e3045fdb8012f0 2023-05-15T17:57:19+02:00 Advantages of the basin approach for investigations of aufeises (naleds) V. V. Shepelev 2016-10-01T00:00:00Z https://doi.org/10.15356/2076-6734-2016-3-381-386 https://doaj.org/article/90cd9d74cdaf4ce895e3045fdb8012f0 RU rus Nauka https://ice-snow.igras.ru/jour/article/view/325 https://doaj.org/toc/2076-6734 https://doaj.org/toc/2412-3765 2076-6734 2412-3765 doi:10.15356/2076-6734-2016-3-381-386 https://doaj.org/article/90cd9d74cdaf4ce895e3045fdb8012f0 Лëд и снег, Vol 56, Iss 3, Pp 381-386 (2016) бассейновый подход коэффициент относительной наледности криолитозона наледеобразование наледь речной бассейн Science Q article 2016 ftdoajarticles https://doi.org/10.15356/2076-6734-2016-3-381-386 2023-03-19T01:40:11Z Formation of aufeises (naleds) is rather widely distributed cryogenic process in the permafrost zone, therefore naleds are reasonably called the seasonal glaciation of the planet. The ever-increasing interest in aufeises significantly extends the thematic focus of studying them. Various methodological approaches (basin, geological-structural, lithologic-facies, statistical, etc.) are used to reveal regularities of the aufeis occurrence. Using several river basins in Yakutia and its territory as the examples, the perspectivity of the basin approach for investigation of the aufeis distribution is substantiated in this study. The results demonstrated the clear relationship between the quantitative indicators of areal distribution of naleds and altitudes of places of their formation for individual river basins. This relationship suggests that aufeises in river basins of the permafrost zones are important elements in the water-balance and water exchange, which is closely interrelated with not only climatic and morphometric characteristics of a basin, but it does also correlate with its hydrological, hydrogeological, geological, geocryological, landscape and other conditions. Article in Journal/Newspaper permafrost Yakutia Directory of Open Access Journals: DOAJ Articles Ice and Snow 56 3 381 386 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
Russian |
topic |
бассейновый подход коэффициент относительной наледности криолитозона наледеобразование наледь речной бассейн Science Q |
spellingShingle |
бассейновый подход коэффициент относительной наледности криолитозона наледеобразование наледь речной бассейн Science Q V. V. Shepelev Advantages of the basin approach for investigations of aufeises (naleds) |
topic_facet |
бассейновый подход коэффициент относительной наледности криолитозона наледеобразование наледь речной бассейн Science Q |
description |
Formation of aufeises (naleds) is rather widely distributed cryogenic process in the permafrost zone, therefore naleds are reasonably called the seasonal glaciation of the planet. The ever-increasing interest in aufeises significantly extends the thematic focus of studying them. Various methodological approaches (basin, geological-structural, lithologic-facies, statistical, etc.) are used to reveal regularities of the aufeis occurrence. Using several river basins in Yakutia and its territory as the examples, the perspectivity of the basin approach for investigation of the aufeis distribution is substantiated in this study. The results demonstrated the clear relationship between the quantitative indicators of areal distribution of naleds and altitudes of places of their formation for individual river basins. This relationship suggests that aufeises in river basins of the permafrost zones are important elements in the water-balance and water exchange, which is closely interrelated with not only climatic and morphometric characteristics of a basin, but it does also correlate with its hydrological, hydrogeological, geological, geocryological, landscape and other conditions. |
format |
Article in Journal/Newspaper |
author |
V. V. Shepelev |
author_facet |
V. V. Shepelev |
author_sort |
V. V. Shepelev |
title |
Advantages of the basin approach for investigations of aufeises (naleds) |
title_short |
Advantages of the basin approach for investigations of aufeises (naleds) |
title_full |
Advantages of the basin approach for investigations of aufeises (naleds) |
title_fullStr |
Advantages of the basin approach for investigations of aufeises (naleds) |
title_full_unstemmed |
Advantages of the basin approach for investigations of aufeises (naleds) |
title_sort |
advantages of the basin approach for investigations of aufeises (naleds) |
publisher |
Nauka |
publishDate |
2016 |
url |
https://doi.org/10.15356/2076-6734-2016-3-381-386 https://doaj.org/article/90cd9d74cdaf4ce895e3045fdb8012f0 |
genre |
permafrost Yakutia |
genre_facet |
permafrost Yakutia |
op_source |
Лëд и снег, Vol 56, Iss 3, Pp 381-386 (2016) |
op_relation |
https://ice-snow.igras.ru/jour/article/view/325 https://doaj.org/toc/2076-6734 https://doaj.org/toc/2412-3765 2076-6734 2412-3765 doi:10.15356/2076-6734-2016-3-381-386 https://doaj.org/article/90cd9d74cdaf4ce895e3045fdb8012f0 |
op_doi |
https://doi.org/10.15356/2076-6734-2016-3-381-386 |
container_title |
Ice and Snow |
container_volume |
56 |
container_issue |
3 |
container_start_page |
381 |
op_container_end_page |
386 |
_version_ |
1766165712649322496 |