气候变化领域集成服务门户(CCPortal): Features of revegetation of drift sand sites in the Northern Taiga subzone of Western Siberia

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DOI	10.21782/KZ1560-7496-2016-3(3-13)
	Features of revegetation of drift sand sites in the Northern Taiga subzone of Western Siberia
	Sizov O.S.; Lobotrosova S.A.
发表日期	2016
ISSN	15607496
卷号	20 期号:3
英文摘要	Despite of the presence of large drift sand sites, the northern taiga areas of Western Siberia are currently experiencing a decrease in deflation processes and increase in self-regeneration of the vegetation cover. This paper discusses the drivers of the formation of sand arenas and analyzes the nature of changes in climatic conditions in the Nadym River downstream area. The results of interpretation of space images made at different times and field observations data allow assessing the vegetation cover and dune microrelief dynamics within the bounds of natural deflation basins widely developed in the study area. The particular characteristics and mechanisms of revegetation are demonstrated by the example of a model deflation basin.
英文关键词	Aeolian processes; Climate; Freeze-thaw action; Vegetation; Western Siberia
学科领域	boreal forest; climate effect; deflation; dune; eolian process; freeze-thaw cycle; microrelief; revegetation; vegetation cover; Nadym Basin; Russian Federation; Siberia
语种	英语
scopus关键词	boreal forest; climate effect; deflation; dune; eolian process; freeze-thaw cycle; microrelief; revegetation; vegetation cover; Nadym Basin; Russian Federation; Siberia
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/119747
作者单位	Earth Cryosphere Institute, SB RAS, Malygina str., 86, Tyumen, 625026, Russian Federation
推荐引用方式 GB/T 7714	Sizov O.S.,Lobotrosova S.A.. Features of revegetation of drift sand sites in the Northern Taiga subzone of Western Siberia[J],2016,20(3).
APA	Sizov O.S.,&Lobotrosova S.A..(2016).Features of revegetation of drift sand sites in the Northern Taiga subzone of Western Siberia.Earth's Cryosphere,20(3).
MLA	Sizov O.S.,et al."Features of revegetation of drift sand sites in the Northern Taiga subzone of Western Siberia".Earth's Cryosphere 20.3(2016).