| Using glacier area ratio to quantify effects of melt water on runoff | |
| Zhang, Yiqing1,2; Luo, Yi1,2,3; Sun, Lin1; Liu, Shiyin4; Chen, Xi3; Wang, Xiaolei1,2 | |
| 刊名 | JOURNAL OF HYDROLOGY
 |
| 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 |
| DOI | 10.1016/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 |
| 出版者 | ELSEVIER SCIENCE BV |
| WOS记录号 | WOS:000378360600023 |
| 内容类型 | 期刊论文 |
| URI标识 | http://www.corc.org.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. |
| 个性服务 |
| 查看访问统计 |
| 相关权益政策 |
| 暂无数据 |
| 收藏/分享 |
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。
修改评论