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DOI | 10.1007/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 |
ISSN | 1674-6767 |
EISSN | 2194-7783 |
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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