DOI: 10.1016/j.gloplacha.2012.12.010
论文题名: Accelerated loss of alpine glaciers in the Kodar Mountains, south-eastern Siberia
作者: Stokes C.R. ; Shahgedanova M. ; Evans I.S. ; Popovnin V.V.
刊名: Global and Planetary Change
ISSN: 0921-8330
出版年: 2013
卷: 101 起始页码: 82
结束页码: 96
语种: 英语
英文关键词: Climate change
; Kodar Mountains
; Mountain glaciers
; Remote sensing
; Russia
Scopus关键词: Alpine glacier
; Anthropogenic climate changes
; Glacier ice
; Glacier inventory
; Kodar Mountains
; Landsat imagery
; Mountain glaciers
; Recent trends
; Rock glaciers
; Russia
; SIBERIA
; Small Sample Size
; Summer warming
; Climate change
; Debris
; Landforms
; Mapping
; Remote sensing
; Shrinkage
; Sun
; Ice
; alpine environment
; anthropogenic effect
; climate change
; glacial environment
; global warming
; Landsat
; mapping method
; remote sensing
; satellite imagery
; solar radiation
; topography
; Kodar Mountains
; Russian Federation
英文摘要: The recession of mountain glaciers around the world has been linked to anthropogenic climate change and small glaciers (e.g. <2km2) are thought to be particularly vulnerable, with reports of their disappearance from several regions. However, the response of small glaciers to climate change can be modulated by non-climatic factors such as topography and debris cover and there remain a number of regions where their recent change has evaded scrutiny. This paper presents results of the first multi-year remote sensing survey of glaciers in the Kodar Mountains, the only glaciers in SE Siberia, which we compare to previous glacier inventories from this continental setting that reported total glacier areas of 18.8km2 in ca. 1963 (12.6km2 of exposed ice) and 15.5km2 in 1974 (12km2 of exposed ice). Mapping their debris-covered termini is difficult but delineation of debris-free ice on Landsat imagery reveals 34 glaciers with a total area of 11.72±0.72km2 in 1995, followed by a reduction to 9.53±0.29km2 in 2001 and 7.01±0.23km2 in 2010. This represents a ~44% decrease in exposed glacier ice between ca. 1963 and 2010, but with 40% lost since 1995 and with individual glaciers losing as much as 93% of their exposed ice. Thus, although continental glaciers are generally thought to be less sensitive than their maritime counterparts, a recent acceleration in shrinkage of exposed ice has taken place and we note its coincidence with a strong summer warming trend in the region initiated at the start of the 1980s. Whilst smaller and shorter glaciers have, proportionally, tended to shrink more rapidly, we find no statistically significant relationship between shrinkage and elevation characteristics, aspect or solar radiation. This is probably due to the small sample size, limited elevation range, and topographic setting of the glaciers in deep valleys-heads. Furthermore, many of the glaciers possess debris-covered termini and it is likely that the ablation of buried ice is lagging the shrinkage of exposed ice, such that a growth in the proportion of debris cover is occurring, as observed elsewhere. If recent trends continue, we hypothesise that glaciers could evolve into a type of rock glacier within the next few decades, introducing additional complexity in their response and delaying their potential demise. © 2012 Elsevier B.V. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84872578668&doi=10.1016%2fj.gloplacha.2012.12.010&partnerID=40&md5=855378f10a710b24fdf965eda477c633
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/11236
Appears in Collections: 全球变化的国际研究计划
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作者单位: Department of Geography, Durham University, Durham, United Kingdom
Recommended Citation:
Stokes C.R.,Shahgedanova M.,Evans I.S.,et al. Accelerated loss of alpine glaciers in the Kodar Mountains, south-eastern Siberia[J]. Global and Planetary Change,2013-01-01,101.