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| DOI | 10.3390/atmos14091360 |
| Spatiotemporal Distribution Characteristics of Actual Evapotranspiration in the Qinghai-Tibet Plateau | |
| Huang, Shan; Xiao, Tiangui; Jia, La; Han, Lin | |
| 发表日期 | 2023 |
| EISSN | 2073-4433 |
| 卷号 | 14期号:9 |
| 英文摘要 | Evapotranspiration is a key part of the water cycle between the atmosphere and the land surface, and it is an important parameter for studying the land-atmosphere system. Change and evolution have important implications. Therefore, the understanding and research of actual evapotranspiration (AET) can profoundly affect water use, ecological environment, temperature, and precipitation. In this paper, the single-layer monthly average reanalysis meteorological data of the Qinghai-Tibet Plateau from 1981 to 2020 was used to study and calculate the actual evapotranspiration in the Qinghai-Tibet Plateau, and the temporal and spatial variation characteristics, variation laws, and changes were analyzed by methods such as cumulative anomalies and the Mann-Kendall trend test. The results showed the following: (1) The evapotranspiration gradually decreased from southeast to northwest. The evapotranspiration in the southeastern region is strong, and the maximum value appears in the Hengduan Mountains. (2) The evapotranspiration was the largest in summer and gradually decreased from southeast to northwest; the evapotranspiration in spring and autumn was relatively uniform, with little overall difference, and the evapotranspiration was the lowest in winter. (3) There were mainly three spatial distribution modes of evapotranspiration in the Qinghai-Tibet Plateau, which were characterized by a significant and consistent change centered on the Tibet region, an east-west reverse type, and an east-west negative-positive-negative of the distributed three-pole space. The corresponding time coefficients characterized the interdecadal and interannual variation, and the decadal variation characteristics are more significant than the annual variation characteristics. (4) The actual evapotranspiration had step change; the step change years were 1989, 2002, 2011, and 2015, and there was an interval of about 5 years. |
| 关键词 | Qinghai-Tibet Plateauactual evapotranspirationspatiotemporal distributionMann-Kendall trend test |
| WOS研究方向 | Environmental Sciences ; Meteorology & Atmospheric Sciences |
| WOS记录号 | WOS:001071119500001 |
| 来源期刊 | ATMOSPHERE
 |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/282570 |
| 作者单位 | Chengdu University of Information Technology; Chengdu University of Information Technology |
| 推荐引用方式 GB/T 7714 | Huang, Shan,Xiao, Tiangui,Jia, La,et al. Spatiotemporal Distribution Characteristics of Actual Evapotranspiration in the Qinghai-Tibet Plateau[J],2023,14(9). |
| APA | Huang, Shan,Xiao, Tiangui,Jia, La,&Han, Lin.(2023).Spatiotemporal Distribution Characteristics of Actual Evapotranspiration in the Qinghai-Tibet Plateau.ATMOSPHERE,14(9). |
| MLA | Huang, Shan,et al."Spatiotemporal Distribution Characteristics of Actual Evapotranspiration in the Qinghai-Tibet Plateau".ATMOSPHERE 14.9(2023). |
| 条目包含的文件 | 条目无相关文件。 | |||||
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