globalchange  > 气候减缓与适应
DOI: 10.1007/s10584-016-1688-z
Scopus记录号: 2-s2.0-84968680138
论文题名:
Distribution, attribution, and radiative forcing of snow cover changes over China from 1982 to 2013
作者: Chen X.; Liang S.; Cao Y.; He T.
刊名: Climatic Change
ISSN: 0165-0009
EISSN: 1573-1480
出版年: 2016
卷: 137, 期:2018-03-04
起始页码: 363
结束页码: 377
语种: 英语
Scopus关键词: Arid regions ; Atmospheric radiation ; Budget control ; Earth (planet) ; Earth atmosphere ; Cooling effects ; Eastern Tibetan plateau ; Positive changes ; Radiative forcings ; Satellite observations ; Significance levels ; Snow cover variations ; Spatial and temporal resolutions ; Snow ; clear sky ; climate change ; energy budget ; precipitation (climatology) ; radiative forcing ; satellite imagery ; snow cover ; spatial distribution ; spatiotemporal analysis ; temperature effect ; China ; Qinghai-Xizang Plateau
英文摘要: Unlike large-scale snow cover variation and its effects on the Earth’s climate system, regional-scale snow cover and its impacts on surface–atmosphere interaction and the Earth’s energy budget have received little attention. This study aims to quantify the distribution and attribution of snow cover changes over mainland China and the associated snow radiative forcing from 1982 to 2013 by using satellite observations at high spatial and temporal resolutions. Driven by decreased temperature and increased precipitation in the accumulation season, the snow cover fraction (SCF) over mainland China shows an increasing trend at 0.29 % decade−1 during 1982–2013, which is significant at the 0.05 level. The spatial distribution of changes in the SCF over the 32-year study period exhibits a maximum positive change of 31.08 % in the south-eastern Tibetan Plateau (TP) zone and a maximum negative change of 27.49 % in the northwestern Xinjiang arid zone as well as in the western margin area of the TP zone. Induced by overall increased SCF over mainland China, the snow radiative forcing (RFsnow) in clear-sky conditions is shown to have strengthened by 0.21 ± 0.01 Wm−2 decade−1 at the 0.05 significance level during 1982–2013, which indicates that the cooling effects caused by snow cover over mainland China have strengthened since 1982. © 2016, The Author(s).
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/84252
Appears in Collections:气候减缓与适应
气候变化事实与影响

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作者单位: State Key Laboratory of Remote Sensing Science, School of Geography, Beijing Normal University, Beijing, China; Department of Geographical Sciences, University of Maryland, College Park, MD, United States

Recommended Citation:
Chen X.,Liang S.,Cao Y.,et al. Distribution, attribution, and radiative forcing of snow cover changes over China from 1982 to 2013[J]. Climatic Change,2016-01-01,137(2018-03-04)
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