Evaluation of the rescaled complementary principle in the estimation of evaporation on the Tibetan Plateau
文献类型:期刊论文
作者 | Yang Wenjing3; Wang Yibo1,3; Liu Xin3; Zhao Haipeng3; Shao Rui3; Wang Genxu2![]() |
刊名 | SCIENCE OF THE TOTAL ENVIRONMENT
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出版日期 | 2020 |
卷号 | 699页码:134367 |
关键词 | Generalized nonlinear complementary relationship Tibetan Plateau Evaporation Maximum apparent potential evaporation |
ISSN号 | 0048-9697 |
DOI | 10.1016/j.scitotenv.2019.134367 |
产权排序 | 3 |
通讯作者 | Wang, Yibo(wangyib@lzu.edu.cn) |
文献子类 | Article |
英文摘要 | Accurate quantification of the terrestrial water balance can improve our knowledge of regional water cycle changes, and deepen our understanding of evaporation in hydrological cycle and under climate change. However, sparse observation networks on the Tibetan Plateau (TP) prevent the reliable estimates of actual evaporation. Based on the China regional surface Meteorological Feature Dataset (CMFD) and the Global Land Surface Satellite (GLASS) product, we adopted the latest rescaled nonlinear complementary relationship (CR) to calculate the monthly actual evaporation (E) from 1982 to 2015. We analyzed the spatio-temporal variability of the annual E on the entire TP, and explored the main meteorological factors controlling the annual E and the regulation of multiyear average annual E in different vegetation zones from southeast to northwest. Our results indicated that the net radiation (R-n) and E exhibited a favorable agreement with monthly changes of the observed values; and E estimated by the CR explained 79-96% variation of the eddy covariance flux measurements. The multiyear average E was 373.12 mm yr (1) and displayed similar spatial patterns of decreasing from southeast to northwest with two remote sensing products (GLDAS_VIC, GLEAM_v3.3) and one hydrological model (Budyko). Additionally, based on the Mann-Kendall trend test, there were 21.56% of the TP with significant upward trend of annual E which mainly distributed in the area with dense glaciers. The Nyenchen Tanglha Mountains and Pamirs Plateau area had the most obvious upward trend, with up to over 6 mm yr(-1). In a relative sense, the key meteorological elements which affected annual E on the TP were relative humidity (RH) (r = 0.63) and R-n (r = 0.56). (C) 2019 Elsevier B.V. All rights reserved. |
电子版国际标准刊号 | 1879-1026 |
WOS关键词 | CLIMATE-CHANGE ; ALPINE GRASSLAND ; PAN EVAPORATION ; 2-SOURCE MODEL ; BARE SOIL ; WATER ; EVAPOTRANSPIRATION ; LAKE ; PERMAFROST ; CHINA |
资助项目 | National Natural Science Foundation of China[41877149] ; National Natural Science Foundation of China[41530752] ; Key Project of National Natural Science Foundation of China[91547203] |
WOS研究方向 | Environmental Sciences & Ecology |
语种 | 英语 |
WOS记录号 | WOS:000500583400085 |
出版者 | ELSEVIER |
资助机构 | National Natural Science Foundation of China ; Key Project of National Natural Science Foundation of China |
源URL | [http://ir.imde.ac.cn/handle/131551/33556] ![]() |
专题 | 成都山地灾害与环境研究所_山地表生过程与生态调控重点实验室 |
通讯作者 | Wang Yibo |
作者单位 | 1.State Key laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences (CAS), Lanzhou 730000, China; 2.Key Laboratory of Mountain Surface Processes and Ecological Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences (CAS), Chengdu 610041, China 3.College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China; |
推荐引用方式 GB/T 7714 | Yang Wenjing,Wang Yibo,Liu Xin,et al. Evaluation of the rescaled complementary principle in the estimation of evaporation on the Tibetan Plateau[J]. SCIENCE OF THE TOTAL ENVIRONMENT,2020,699:134367. |
APA | Yang Wenjing,Wang Yibo,Liu Xin,Zhao Haipeng,Shao Rui,&Wang Genxu.(2020).Evaluation of the rescaled complementary principle in the estimation of evaporation on the Tibetan Plateau.SCIENCE OF THE TOTAL ENVIRONMENT,699,134367. |
MLA | Yang Wenjing,et al."Evaluation of the rescaled complementary principle in the estimation of evaporation on the Tibetan Plateau".SCIENCE OF THE TOTAL ENVIRONMENT 699(2020):134367. |
入库方式: OAI收割
来源:成都山地灾害与环境研究所
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