Glaciers of the northern massif of the Suntar-Khayata Mountains: current state and dynamics since the end of 1950s

The estimation of glaciers of the Suntar-Khayata Mountains (the Northeastern Siberia) in the context of previously published data is presented. Under the background of current warming the glaciers in this region retreat enough quickly, they decrease not only in a real size, but also by the ice thick...

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Main Authors: B. R. Mavlyudov, M. D. Ananicheva
Format: Article
Language:Russian
Published: Nauka 2016-10-01
Series:Лëд и снег
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/322
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author B. R. Mavlyudov
M. D. Ananicheva
author_facet B. R. Mavlyudov
M. D. Ananicheva
author_sort B. R. Mavlyudov
collection DOAJ
description The estimation of glaciers of the Suntar-Khayata Mountains (the Northeastern Siberia) in the context of previously published data is presented. Under the background of current warming the glaciers in this region retreat enough quickly, they decrease not only in a real size, but also by the ice thickness. In this paper the mean summer temperature and solid precipitation of the key factors for glaciation, which indicate unfavorable conditions for the glacier existence at present time are presented as spatial distribution of trends (for 45 years, until 2012). The glaciers of the northern massif of the Suntar-Khayata have a negative ice mass balance as their entire surface is below the equilibrium line altitude. Mean thickness of superimposed ice on the glaciers of this massif was about 17 cm. Based on the assumption of climate variation in the Northern Pacific data it is suggested about the beginning of more favorable climatic conditions for the Suntar-Khayata glaciers.
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institution Kabale University
issn 2076-6734
2412-3765
language Russian
publishDate 2016-10-01
publisher Nauka
record_format Article
series Лëд и снег
spelling doaj-art-d85d5268ff274e33aad87363da12a1952025-08-20T03:37:50ZrusNaukaЛëд и снег2076-67342412-37652016-10-0156334535710.15356/2076-6734-2016-3-345-357278Glaciers of the northern massif of the Suntar-Khayata Mountains: current state and dynamics since the end of 1950sB. R. Mavlyudov0M. D. Ananicheva1Institute of Geography, Russian Academy of SciencesInstitute of Geography, Russian Academy of SciencesThe estimation of glaciers of the Suntar-Khayata Mountains (the Northeastern Siberia) in the context of previously published data is presented. Under the background of current warming the glaciers in this region retreat enough quickly, they decrease not only in a real size, but also by the ice thickness. In this paper the mean summer temperature and solid precipitation of the key factors for glaciation, which indicate unfavorable conditions for the glacier existence at present time are presented as spatial distribution of trends (for 45 years, until 2012). The glaciers of the northern massif of the Suntar-Khayata have a negative ice mass balance as their entire surface is below the equilibrium line altitude. Mean thickness of superimposed ice on the glaciers of this massif was about 17 cm. Based on the assumption of climate variation in the Northern Pacific data it is suggested about the beginning of more favorable climatic conditions for the Suntar-Khayata glaciers.https://ice-snow.igras.ru/jour/article/view/322air temperaturealbedodescent of glacier surfaceglacierglacier degradationmass balance of glacierprecipitationsuntar-khayata mountainsthe elathe northeastern siberia
spellingShingle B. R. Mavlyudov
M. D. Ananicheva
Glaciers of the northern massif of the Suntar-Khayata Mountains: current state and dynamics since the end of 1950s
Лëд и снег
air temperature
albedo
descent of glacier surface
glacier
glacier degradation
mass balance of glacier
precipitation
suntar-khayata mountains
the ela
the northeastern siberia
title Glaciers of the northern massif of the Suntar-Khayata Mountains: current state and dynamics since the end of 1950s
title_full Glaciers of the northern massif of the Suntar-Khayata Mountains: current state and dynamics since the end of 1950s
title_fullStr Glaciers of the northern massif of the Suntar-Khayata Mountains: current state and dynamics since the end of 1950s
title_full_unstemmed Glaciers of the northern massif of the Suntar-Khayata Mountains: current state and dynamics since the end of 1950s
title_short Glaciers of the northern massif of the Suntar-Khayata Mountains: current state and dynamics since the end of 1950s
title_sort glaciers of the northern massif of the suntar khayata mountains current state and dynamics since the end of 1950s
topic air temperature
albedo
descent of glacier surface
glacier
glacier degradation
mass balance of glacier
precipitation
suntar-khayata mountains
the ela
the northeastern siberia
url https://ice-snow.igras.ru/jour/article/view/322
work_keys_str_mv AT brmavlyudov glaciersofthenorthernmassifofthesuntarkhayatamountainscurrentstateanddynamicssincetheendof1950s
AT mdananicheva glaciersofthenorthernmassifofthesuntarkhayatamountainscurrentstateanddynamicssincetheendof1950s