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	Siberian glaciers as a component of cryolithogenic-glacial geosystems
	Sheinkman V.S.; Melnikov V.P.
发表日期	2014
ISSN	15607496
卷号	18 期号:2
英文摘要	Cold continental climate in Siberia determines peculiar conditions of glacier formation and dynamics. Interacting with permafrost, they become a new element of cryodiversity, i. e. a set of objects and phenomena produced by cold, and differ greatly from the glaciers which are considered from the classical positions of the Alpine glaciation model. On cooling down to quite low temperatures (far below 0 °C), the glaciers in Siberia acquire traits which are more inherent for the permafrost rather than for Alpine-type glaciers. The acquired feature calls for regarding the formed aggregation of glaciers and permafrost as peculiar geosystems; the authors name them cryolithogenic-glacial systems.
英文关键词	Cryolithozone; Glaciation; Interaction of permafrost and glaciers
学科领域	alpine environment; cooling; glaciation; glacier dynamics; glaciology; low temperature
语种	英语
scopus关键词	alpine environment; cooling; glaciation; glacier dynamics; glaciology; low temperature
来源期刊	Earth's Cryosphere
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/120207
作者单位	Earth Cryosphere Institute, SB RAS, P/O Box 1230, Tyumen, 625000, Russian Federation; Tyumen State Oil and Gas University, Volodarskogo Str., 36, Tyumen, 625000, Russian Federation
推荐引用方式 GB/T 7714	Sheinkman V.S.,Melnikov V.P.. Siberian glaciers as a component of cryolithogenic-glacial geosystems[J],2014,18(2).
APA	Sheinkman V.S.,&Melnikov V.P..(2014).Siberian glaciers as a component of cryolithogenic-glacial geosystems.Earth's Cryosphere,18(2).
MLA	Sheinkman V.S.,et al."Siberian glaciers as a component of cryolithogenic-glacial geosystems".Earth's Cryosphere 18.2(2014).