中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Reduced winter runoff in a mountainous permafrost region in the northern Tibetan Plateau

文献类型:期刊论文

作者Gao, Tanguang1; Zhang, Tingjun1; Cao, Lin1; Kang, Shichang2,3; Sillanpaa, Mika4
刊名COLD REGIONS SCIENCE AND TECHNOLOGY
出版日期2016-06-01
卷号126页码:36-43
关键词Hydrological regime Permafrost degradation Runoff Climate change Tibetan Plateau
ISSN号0165-232X
DOI10.1016/j.coldregions.2016.03.007
通讯作者Gao, Tanguang(gaotanguang@163.com)
英文摘要The degradation of mountain permafrost under climate warming may alter the runoff regime of high mountainous catchments. In this study, we evaluated the influence of permafrost on the hydrological regime using hydrological signals in the Yeniugou Basin located in a mountainous permafrost region in the Qilian Mountains of the northern Tibetan Plateau (TP). The effect of permafrost degradation on the hydrological response was assessed based on 28 years of runoff and meteorological data. The results indicated that the investigated region exhibited a large increase in annual surface ground temperature from 1979 to 2006, with almost unchanged precipitation and evaporation potential. The winter runoff levels exhibited a significant decreasing linear trend, whereas the annual runoff and runoff in other seasons did not show any distinct linear trends. According to a comprehensive analysis of the relationships between winter runoff and meteorological factors, the ratio of maximum(Q(max)) and minimum (Q(min)) discharge, the recession coefficient and baseflow separation, and the reduced winter runoff were significantly correlated with thawing of permafrost. However, due to a time-lag response of climate forcing to permafrost thawing, some of these changes are undetectable over a short period. This study provides preliminary data on cold region hydrology and its response to climate change. (C) 2016 Elsevier B.V. All rights reserved.
收录类别SCI
WOS关键词HEIHE RIVER-BASIN ; ACTIVE-LAYER THICKNESS ; NORTHWEST CHINA ; CLIMATE-CHANGE ; SWAT MODEL ; BASEFLOW ; FLOW ; HYDROLOGY ; ALASKA ; INDEX
WOS研究方向Engineering ; Geology
WOS类目Engineering, Environmental ; Engineering, Civil ; Geosciences, Multidisciplinary
语种英语
WOS记录号WOS:000374992400005
出版者ELSEVIER SCIENCE BV
URI标识http://www.irgrid.ac.cn/handle/1471x/2557326
专题寒区旱区环境与工程研究所
通讯作者Gao, Tanguang
作者单位1.Lanzhou Univ, Coll Earth & Environm Sci, Minist Educ, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China
2.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Cryospher Sci, Lanzhou 730000, Peoples R China
3.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
4.Lappeenranta Univ Technol, Lab Green Chem, Sammonkatu 12, FI-50130 Mikkeli, Finland
推荐引用方式
GB/T 7714
Gao, Tanguang,Zhang, Tingjun,Cao, Lin,et al. Reduced winter runoff in a mountainous permafrost region in the northern Tibetan Plateau[J]. COLD REGIONS SCIENCE AND TECHNOLOGY,2016,126:36-43.
APA Gao, Tanguang,Zhang, Tingjun,Cao, Lin,Kang, Shichang,&Sillanpaa, Mika.(2016).Reduced winter runoff in a mountainous permafrost region in the northern Tibetan Plateau.COLD REGIONS SCIENCE AND TECHNOLOGY,126,36-43.
MLA Gao, Tanguang,et al."Reduced winter runoff in a mountainous permafrost region in the northern Tibetan Plateau".COLD REGIONS SCIENCE AND TECHNOLOGY 126(2016):36-43.

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来源:寒区旱区环境与工程研究所

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