Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1029/2018JD028459 |
Measurements and Modeling of the Water Budget in Semiarid High-Altitude Qinghai Lake Basin, Northeast Qinghai-Tibet Plateau | |
Ma, Yu-Jun1,2,3; Li, Xiao-Yan1,2; Liu, Lei2; Huang, Yong-Mei1,2; Li, Zhou2; Hu, Xia1,2; Wu, Xiu-Chen1,2; Yang, Xiao-Fan1,2; Wang, Pei1,2; Zhao, Shao-Jie1,2; Zhang, Guang-Hui1,4; Liu, Bao-Yuan1,4 | |
2018-10-16 | |
发表期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
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ISSN | 2169-897X |
EISSN | 2169-8996 |
出版年 | 2018 |
卷号 | 123期号:19页码:10857-10871 |
文章类型 | Article |
语种 | 英语 |
国家 | Peoples R China |
英文摘要 | Water budget plays an important role in ecological functions and biogeochemical cycles on the Qinghai-Tibet Plateau (QTP). However, the key factors that govern the water budget across spatiotemporal scales in natural conditions are poorly understood, especially in the alpine region. To advance our understanding of how and why the water budget varies at the ecosystem and catchment scales, this study measured and modeled the main water budget components in the Qinghai Lake Basin (QLB) and further investigated the key factors for evapotranspiration and streamflow. The results showed that most monthly precipitation from June to September was greater than the corresponding evapotranspiration from the high-altitude Kobresia meadow (KMd.) and Potentilla fruticosa shrub (PFSh.) ecosystem, and vice versa for the low-altitude Achnatherum splendens steppe (ASSt.) ecosystem. The mean annual proportions of evapotranspiration of precipitation for the KMd., PFSh., and ASSt. ecosystems were 0.83, 1.06, and 1.02, respectively, from 2014 to 2015. The study highlights that the high-altitude KMd. ecosystem is the main contributing area for runoff generation in the QLB. From ASSt. to PFSh. and then to the KMd. ecosystem, the key factors for evapotranspiration switched from water conditions to temperature conditions with the increase in elevation. The future scenario of climate warming and precipitation increase may cause a rise in evapotranspiration and streamflow in the QLB. Moreover, the increasing precipitation may be consumed mainly by evapotranspiration in the high altitude with low slope and by transfer into streamflow in the area with high slope. |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000448374800004 |
WOS关键词 | RIVER-BASIN ; SURFACE-ENERGY ; LOESS PLATEAU ; ALPINE MEADOW ; SOIL-WATER ; EVAPOTRANSPIRATION ; ECOSYSTEM ; BALANCE ; CLIMATE ; VEGETATION |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/33073 |
专题 | 气候变化 |
作者单位 | 1.Beijing Normal Univ, Fac Geog Sci, State Key Lab Earth Surface Proc & Resource Ecol, Beijing, Peoples R China; 2.Beijing Normal Univ, Sch Nat Resources, Fac Geog Sci, Beijing, Peoples R China; 3.Sun Yat Sen Univ, Sch Geog & Planning, Guangzhou, Guangdong, Peoples R China; 4.Beijing Normal Univ, Sch Geog, Fac Geog Sci, Beijing, Peoples R China |
推荐引用方式 GB/T 7714 | Ma, Yu-Jun,Li, Xiao-Yan,Liu, Lei,et al. Measurements and Modeling of the Water Budget in Semiarid High-Altitude Qinghai Lake Basin, Northeast Qinghai-Tibet Plateau[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2018,123(19):10857-10871. |
APA | Ma, Yu-Jun.,Li, Xiao-Yan.,Liu, Lei.,Huang, Yong-Mei.,Li, Zhou.,...&Liu, Bao-Yuan.(2018).Measurements and Modeling of the Water Budget in Semiarid High-Altitude Qinghai Lake Basin, Northeast Qinghai-Tibet Plateau.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,123(19),10857-10871. |
MLA | Ma, Yu-Jun,et al."Measurements and Modeling of the Water Budget in Semiarid High-Altitude Qinghai Lake Basin, Northeast Qinghai-Tibet Plateau".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 123.19(2018):10857-10871. |
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