中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Using glacier area ratio to quantify effects of melt water on runoff

文献类型:期刊论文

作者Zhang, Yiqing1,2; Luo, Yi1,2,3; Sun, Lin1; Liu, Shiyin4; Chen, Xi3; Wang, Xiaolei1,2
刊名JOURNAL OF HYDROLOGY
出版日期2016-07-01
卷号538页码:269-277
关键词Glacier area ratio Glacier melt Runoff coefficient Coefficient of variation of runoff SWAT
ISSN号0022-1694
DOI10.1016/j.jhydrol.2016.04.026
通讯作者Luo, Yi(luoyi@igsnrr.ac.cn)
英文摘要Twenty-four headwater catchments with varying glacier area ratios (GARs) in the Eastern and Central Tian Shan Mountains were simulated by the glacier-enhanced Soil and Water Assessment Tool (SWAT) model from 1961 to 2007. The mean catchment GAR ranges between 0.7% and 44.8% with a mean of 8.6%. Through synthetic analysis of the glacio-hydrological processes simulation results of the catchments, it was found that the GAR is an effective index that can be used to interpret quantitatively the varying influences of glaciers on runoff across catchments. Among the twenty-four catchments, the ratio of glacier melt contribution (RGMC) to runoff varies between 3.5% and 67.5% with a mean of 24.0%; the ratio of ice melt contribution (RIMC) between 1.4% and 35.8% with a mean of 10.5%; the ratio of ice melt in glacier melt between 33.4% and 59.1% with a mean of 43.4%; the runoff coefficient (RC) between 0.24 and 0.90 with a mean of 0.52; and the coefficient of variation (CV) of runoff between 0.10 and 0.29 with a mean of 0.18. Based on synthetic analysis, it was found that (1) power functions fit the relations between RGMC, RIMC, RC, and CV and GAR with high certainty; (2) the CV decreases with increasing GAR while others increase; and (3) these power functions change sensitively with GAR when GAR is less than 10%, implicating that a small change in GAR may cause remarkable changes in RGMC, RIMC, RC, and CV in the less glacierized catchments. (C) 2016 Published by Elsevier B.V.
收录类别SCI
WOS关键词CLIMATE-CHANGE ; RIVER-BASIN ; NORTHWEST CHINA ; CENTRAL-ASIA ; TIANSHAN MOUNTAINS ; TIEN-SHAN ; PRECIPITATION ; STREAMFLOW ; SNOWMELT ; SIMULATION
WOS研究方向Engineering ; Geology ; Water Resources
WOS类目Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources
语种英语
WOS记录号WOS:000378360600023
出版者ELSEVIER SCIENCE BV
URI标识http://www.irgrid.ac.cn/handle/1471x/2557249
专题寒区旱区环境与工程研究所
通讯作者Luo, Yi
作者单位1.Chinese Acad Sci, Key Lab Ecosyst Network Observat & Modeling, Inst Geog Sci & Nat Resources Res, 11A,Datun Rd, Beijing 100101, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Urumqi 830011, Peoples R China
4.Chinese Acad Sci, State Key Lab Cryospher Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Yiqing,Luo, Yi,Sun, Lin,et al. Using glacier area ratio to quantify effects of melt water on runoff[J]. JOURNAL OF HYDROLOGY,2016,538:269-277.
APA Zhang, Yiqing,Luo, Yi,Sun, Lin,Liu, Shiyin,Chen, Xi,&Wang, Xiaolei.(2016).Using glacier area ratio to quantify effects of melt water on runoff.JOURNAL OF HYDROLOGY,538,269-277.
MLA Zhang, Yiqing,et al."Using glacier area ratio to quantify effects of melt water on runoff".JOURNAL OF HYDROLOGY 538(2016):269-277.

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来源:寒区旱区环境与工程研究所

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