Runoff and sediment yield in relation to precipitation,temperature and glaciers on the Tibetan Plateau  

作　　者：Fan Zhang Chen Zeng Guanxing Wang Li Wang Xiaonan Shi 

机构地区：[1]Key Laboratory of Tibetan Environment Changes and Land Surface Processes,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing,100101,China [2]CAS Center for Excellence in Tibetan Plateau Earth Sciences,Beijing,100101,China [3]University of Chinese Academy of Sciences,Beijing,100101,China

出　　处：《International Soil and Water Conservation Research》2022年第2期197-207,共11页国际水土保持研究（英文）

基　　金：the National Natural Science Foundation of China(Grant No.41877081);the West Light Foun-dation of Interdisciplinary Team,Chinese Academy of Sciences and the Second Tibetan Plateau Scientific Expedition and Research Program(2019QZKK0203)。

摘　　要：The riverine sediment is an essential carrier for nutrients and pollutants delivery and is considered as an important indicator of land degradation and environmental changes.With growing interest in envi-ronmental changes over the Tibetan Plateau,this study investigated mean annual runoff and sediment yield from eight headwater catchments in relation to annual precipitation,air temperature,and glacier area ratio,etc.Results show that runoff(Q)is positively correlated with both precipitation(P)and temperature(T),i.e.,Q¼0.357Pþ20.3T-6.4,indicating combined water supply from rainfall and melt-water,increase of which may exceed the evapotranspiration water loss caused by temperature raise.Sediment yield(S)shows an inverted parabolic relationship with precipitation and at the same time positive correlation with glacier area ratio(Ag),i.e.,S¼0.000609 P2-0.470Pþ48.5 Agþ202.53,indicating that sediment yield is a minimum at about 500e600 mm of precipitation,increasing sharply on both sides of this minimum in one case owing to decreased vegetation protection and in the other to enhanced erosive power and that erosion rate in the glacierized area is generally higher than non-glacierized area.The variation in sediment yield with precipitation can be explained by the operation of two factors,i.e.,rainfall erosive action that increases continuously with increase in precipitation,and vegetation protective action that is unity for zero precipitation and decreases with increases in precip-itation.The above results may be useful in visualizing not only variations in rates of erosion among climatic zones on the Tibetan Plateau but also the probable changes of erosion during a climatic change.

关 键 词：Alpine catchment Climate condition Glacier erosion RUNOFF Sediment yield 

分 类 号：S157[农业科学—土壤学]