Long-term fluctuations of snow cover thickness and maximum snow storage in Gis-Baikal area

The paper describes the variability of snow depth and maximal snow storage at level of biogeographical areas and provinces for the long-term period of 1961–2010. Tendencies of snow depth changes increase in most cases with significant factors of regression, but the changes are rather small, only 0.6...

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Main Author: E. V. Maksyutova
Format: Article
Language:Russian
Published: Nauka 2015-04-01
Series:Лëд и снег
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/99
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author E. V. Maksyutova
author_facet E. V. Maksyutova
author_sort E. V. Maksyutova
collection DOAJ
description The paper describes the variability of snow depth and maximal snow storage at level of biogeographical areas and provinces for the long-term period of 1961–2010. Tendencies of snow depth changes increase in most cases with significant factors of regression, but the changes are rather small, only 0.6–6 cm/10 years. Steady changes of maximal snow storage are positive in the most cases of wood sites. The greatest increase of maximal snow storage on wood sites is noted in the South Siberian mountain and taiga area with 10–21 mm/10 years, and, on the contrary, with 4–8 mm/10 years on field sites of Mid-Siberian taiga area.
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institution Kabale University
issn 2076-6734
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publishDate 2015-04-01
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record_format Article
series Лëд и снег
spelling doaj-art-99c58d80673342a0855f35a6f9d18b592025-08-20T03:59:49ZrusNaukaЛëд и снег2076-67342412-37652015-04-01532404710.15356/2076-6734-2013-2-40-4793Long-term fluctuations of snow cover thickness and maximum snow storage in Gis-Baikal areaE. V. Maksyutova0Sochava Institute of Geography, Siberian Branch of the Russian Academy of Sciences, IrkutskThe paper describes the variability of snow depth and maximal snow storage at level of biogeographical areas and provinces for the long-term period of 1961–2010. Tendencies of snow depth changes increase in most cases with significant factors of regression, but the changes are rather small, only 0.6–6 cm/10 years. Steady changes of maximal snow storage are positive in the most cases of wood sites. The greatest increase of maximal snow storage on wood sites is noted in the South Siberian mountain and taiga area with 10–21 mm/10 years, and, on the contrary, with 4–8 mm/10 years on field sites of Mid-Siberian taiga area.https://ice-snow.igras.ru/jour/article/view/99maximal snow storagepermanent snowstaketendencies of the long-term changessnow depthsnow survey.
spellingShingle E. V. Maksyutova
Long-term fluctuations of snow cover thickness and maximum snow storage in Gis-Baikal area
Лëд и снег
maximal snow storage
permanent snowstake
tendencies of the long-term changes
snow depth
snow survey.
title Long-term fluctuations of snow cover thickness and maximum snow storage in Gis-Baikal area
title_full Long-term fluctuations of snow cover thickness and maximum snow storage in Gis-Baikal area
title_fullStr Long-term fluctuations of snow cover thickness and maximum snow storage in Gis-Baikal area
title_full_unstemmed Long-term fluctuations of snow cover thickness and maximum snow storage in Gis-Baikal area
title_short Long-term fluctuations of snow cover thickness and maximum snow storage in Gis-Baikal area
title_sort long term fluctuations of snow cover thickness and maximum snow storage in gis baikal area
topic maximal snow storage
permanent snowstake
tendencies of the long-term changes
snow depth
snow survey.
url https://ice-snow.igras.ru/jour/article/view/99
work_keys_str_mv AT evmaksyutova longtermfluctuationsofsnowcoverthicknessandmaximumsnowstorageingisbaikalarea