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DOI10.1007/s40333-023-0066-8
Wind regime features and their impacts on the middle reaches of the Yarlung Zangbo River on the Tibetan Plateau, China
Zhang, Yan; Zhang, Zhengcai; Ma, Pengfei; Pan, Kaijia; Zha, Duo; Chen, Dingmei; Shen, Caisheng; Liang, Aimin
发表日期2023
ISSN1674-6767
EISSN2194-7783
起始页码1174
结束页码1195
卷号15期号:10
英文摘要The wide valley of the Yarlung Zangbo River is one of the most intense areas in terms of aeolian activity on the Tibetan Plateau, China. In the past, the evaluation of the intensity of aeolian activity in the Qushui-Sangri section of the Yarlung Zangbo River Valley was mainly based on data from the old meteorological stations, especially in non-sandy areas. In 2020, six new meteorological stations, which are closest to the new meteorological stations, were built in the wind erosion source regions (i.e., sandy areas) in the Qushui-Sangri section. In this study, based on mathematical statistics and empirical orthogonal function (EOF) decomposition analysis, we compared the difference of the wind regime between new meteorological stations and old meteorological stations from December 2020 to November 2021, and discussed the reasons for the discrepancy. The results showed that sandy and non-sandy areas differed significantly regarding the mean velocity (8.3 (& PLUSMN;0.3) versus 7.7 (& PLUSMN;0.3) m/s, respectively), frequency (12.9% (& PLUSMN;6.2%) versus 2.9% (& PLUSMN;1.9%), respectively), and dominant direction (nearly east or west versus nearly north or south, respectively) of sand-driving winds, drift potential (168.1 (& PLUSMN;77.3) versus 24.0 (& PLUSMN;17.9) VU (where VU is the vector unit), respectively), resultant drift potential (92.3 (& PLUSMN;78.5) versus 8.7 (& PLUSMN;9.2) VU, respectively), and resultant drift direction (nearly westward or eastward versus nearly southward or northward, respectively). This indicated an obvious spatial variation in the wind regime between sandy and non-sandy areas and suggested that there exist problems when using wind velocity data from non-sandy areas to evaluate the wind regime in sandy areas. The wind regime between sandy and non-sandy areas differed due to the differences in topography, heat flows, and their coupling with underlying surface, thereby affecting the local atmospheric circulation. Affected by large-scale circulations (westerly jet and Indian monsoon systems), both sandy and non-sandy areas showed similar seasonal variations in their respective wind regime. These findings provide a credible reference for re-understanding the wind regime and scientific wind-sand control in the middle reaches of the Yarlung Zangbo River Valley.
关键词wind regimeaeolian activitysand-driving windsdrift potentialatmospheric circulationYarlung Zangbo RiverTibetan Plateau
英文关键词NORTHERN CHINA; AIR-POLLUTION; DESERT; DUST; LAND; GEOMORPHOLOGY; BASIN; DUNES; SAND
WOS研究方向Environmental Sciences
WOS记录号WOS:001064525900001
来源期刊JOURNAL OF ARID LAND
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/283720
作者单位Chinese Academy of Sciences; Institute of Atmospheric Physics, CAS; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS; Chinese Academy of Sciences; Shaanxi Normal University
推荐引用方式
GB/T 7714
Zhang, Yan,Zhang, Zhengcai,Ma, Pengfei,et al. Wind regime features and their impacts on the middle reaches of the Yarlung Zangbo River on the Tibetan Plateau, China[J],2023,15(10).
APA Zhang, Yan.,Zhang, Zhengcai.,Ma, Pengfei.,Pan, Kaijia.,Zha, Duo.,...&Liang, Aimin.(2023).Wind regime features and their impacts on the middle reaches of the Yarlung Zangbo River on the Tibetan Plateau, China.JOURNAL OF ARID LAND,15(10).
MLA Zhang, Yan,et al."Wind regime features and their impacts on the middle reaches of the Yarlung Zangbo River on the Tibetan Plateau, China".JOURNAL OF ARID LAND 15.10(2023).
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