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Spatial–temporal variation and periodic change in streamflow and suspended sediment discharge along the mainstream of the Yellow River during 1950‐2013
文献类型：期刊论文
| 作者 | Yanhong Wei1; Juying Jiao1,2; Guangju Zhao1,2; Hengkang Zhao2; Zhong He1,2; Xingmin Mu1,2 |
| 刊名 | Catena
 |
| 出版日期 | 2016 |
| 期号 | 140页码:105-115 |
| 通讯作者邮箱 | jyjiao@ms.iswc.ac.cn |
| 关键词 | Streamflow Suspended sediment discharge Spatial–temporal variation Periodic change Yellow River |
| 通讯作者 | Juying Jiao |
| 英文摘要 | Objectives: Under the background of global climate change, variations in streamflow and sediment discharge in the Yellow River would continue with intensified human activities and changes in the ecological environment. To harness the Yellow River, analyzing the degrees of change and the reasons for the streamflow and sediment discharge, as well as predicting the future trends, are urgently needed. Methods: In this paper, the non-parametric Mann–Kendall test, Sen's estimator of slope, Pettitt's test and wavelet transform were applied to detect the trends, the magnitude of the trends and the abrupt changes and periodic variation in streamflow and suspended sediment discharge at eight hydrological stations from 1950 to 2013 along the mainstream of the Yellow River. Results: Over the past 64 years (1950–2013), the spatial distribution of the annual average streamflow was of the“M” type, and the annual average suspended sediment discharge had a parabolic curve shape along the mainstream of the Yellow River. The temporal variation showed a distinct decreasing trend in streamflow since the 1990s and in suspended sediment discharge since the 1980s. Many cycles of oscillations occurred in the streamflow and suspended sediment discharge variation, leading to an alternate change in the wet/dry periods and the high/low sediment discharge periods. Conclusions: In various regions of the Yellow River Basin since the 1970s, climate changes contributed reductions of 17.0–45.0% and 12.2–50.3% for streamflow and suspended sediment discharge, respectively, whereas human activities contributed reductions of 55.0–83.0% and 49.7–87.8%. Therefore, human activities were the major causes of the significant decline in the streamflow and the suspended sediment discharge of the Yellow River over the past six decades. Reasonable and possible measures should be taken to achieve water resources optimization and configuration and to promote watershed management and sustainability in the regions of the Yellow River Basin. |
| 语种 | 英语 |
| WOS记录号 | WOS:000372387100012 |
| 源URL | [http://ir.iswc.ac.cn/handle/361005/7800]  |
| 专题 | 水土保持研究所_水保所科研产出--SCI_2016--SCI |
| 作者单位 | 1.State Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, 26 Xinong Road, Yangling 712100, Shaanxi Province, China 2.Institute of Soil and Water Conservation, Northwest A&F University, 26 Xinong Road, Yangling 712100, Shaanxi Province, China |
| 推荐引用方式 GB/T 7714 | Yanhong Wei,Juying Jiao,Guangju Zhao,et al. Spatial–temporal variation and periodic change in streamflow and suspended sediment discharge along the mainstream of the Yellow River during 1950‐2013[J]. Catena,2016(140):105-115. |
| APA | Yanhong Wei,Juying Jiao,Guangju Zhao,Hengkang Zhao,Zhong He,&Xingmin Mu.(2016).Spatial–temporal variation and periodic change in streamflow and suspended sediment discharge along the mainstream of the Yellow River during 1950‐2013.Catena(140),105-115. |
| MLA | Yanhong Wei,et al."Spatial–temporal variation and periodic change in streamflow and suspended sediment discharge along the mainstream of the Yellow River during 1950‐2013".Catena .140(2016):105-115. |
入库方式： OAI收割
来源：水土保持研究所
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