Sand supplement characteristics indicated by the area of river inland, flood plain in the riverbed of the Yarlung Zangbo River
Pengfei Ma1(), Qunpei Lunzhu2, Yan Zhang3, Nima Ciren2, Junfeng Lu3, Aimin Liang4, Zhengcai Zhang3()
1.Tibet Climate Center,Lhasa 850000,China 2.Shannan Meteorological Bureau,Shannan 856000,Tibet,China 3.Key Laboratory of Desert and Desertification,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China 4.Shanxi Normal University,Xi’an 710119,China
Pengfei Ma, Qunpei Lunzhu, Yan Zhang, Nima Ciren, Junfeng Lu, Aimin Liang, Zhengcai Zhang. Sand supplement characteristics indicated by the area of river inland, flood plain in the riverbed of the Yarlung Zangbo River[J]. Journal of Desert Research, 2021, 41(3): 25-33.
Fig.2 Variation of monthly wind speed, temperature, humidity and rainfall
Fig.2 Variation of monthly wind speed, temperature, humidity and rainfall
Fig.3 Variation of annual average wind velocity (A), annual average threshold wind velocity (B) and annual frequency of threshold wind velocity (C) in five sub-regions
Fig.3 Variation of annual average wind velocity (A), annual average threshold wind velocity (B) and annual frequency of threshold wind velocity (C) in five sub-regions
Fig.4 The development of riverbed, flood plain and river inland area in March (A), May (B), August (C) and November (D)
Fig.4 The development of riverbed, flood plain and river inland area in March (A), May (B), August (C) and November (D)
Table 2 The area of the riverbed, flood plain and river inland in March, May, August and November
Sun J M,Li S H,Muhs D R,et al.Loess sedimentation in Tibet:provenance,processes,and link with Quaternary glaciations[J].Quaternary Science Reviews,2007,26(17/18):2265-2280.
3
Péwé T L,Liu T S,Slatt R M,et al.Origin and Character of Loesslike Silt in the Southern Qinghai-Xizang(Tibet)Plateau,China[M]//Denver,USA:US Geological Survey,1995.