Challenge of vegetation greening on water resources sustainability: Insights from a modeling-based analysis in Northwest China

被引:23
|
作者
Tian, Fei [1 ,2 ,3 ]
Lu, Yi He [2 ]
Fu, Bo Jie [2 ]
Zhang, Lu [3 ]
Zang, Chuan Fu [4 ]
Yang, Yong Hui [5 ]
Qiu, Guo Yu [6 ]
机构
[1] China Agr Univ, Ctr Agr Water Res China, Beijing, Peoples R China
[2] Chinese Acad Sci, Res Ctr Ecoenvironm Sci, State Key Lab Urban & Reg Ecol, Beijing 100085, Peoples R China
[3] CSIRO Land & Water Flagship, Canberra, ACT, Australia
[4] Inner Mongolia Agr Univ, Forestry Coll, Hohhot, Peoples R China
[5] Chinese Acad Sci, Inst Genet & Dev Biol, Ctr Agr Resources Res, Key Lab Agr Water Resources, Shijiazhuang, Peoples R China
[6] Peking Univ, Sch Environm & Energy, Key Lab Urban Habitat Environm Sci & Technol, Shenzhen, Peoples R China
基金
中国国家自然科学基金;
关键词
mountain ecosystem; streamflow; the SWAT model; vegetation greening; water resources sustainability; UNCERTAINTY ANALYSIS; LOESS-PLATEAU; UPPER REACHES; HEIHE RIVER; CLIMATE; YIELD; AFFORESTATION; IMPACTS; FOREST; BASIN;
D O I
10.1002/hyp.11118
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Forest restoration policies are often implemented without the assessment of their full environmental impact. In this study, we investigated the challenges of vegetation greening resulted from forest restoration on water resource sustainability, using a model-based simulation in northwestern China. Four different vegetation scenarios and 25 future climate scenarios were employed using the Soil and Water Assessment Tool model. Results suggest that (a) the mean annual evapotranspiration changes from only 7.2% in the barren case to 100% in the forest case; however, it produced a 35.2% reduction in average annual streamflow and a 157% increase in soil water storage. The upstream vegetation greening caused the enhancement of water retention, while also creating great challenges for future downstream water resource sustainability; (b) seasonal effect was significant in that 100% forest case increased evapotranspiration (+40%) but it also reduced the streamflow (-73%) compared to the barren case in growing season, which may exacerbate spring and summer drought; (c) changes of evapotranspiration and streamflow were only 0.3% and -0.9% at T + 3.9 degrees C when compared to the historic scenario in barren cases, while for all forest cases, variations were 3% and -21.8%, respectively; (d) vegetation greening induced more remarkable changes in hydrological components than those resulting from climate change. Our "what if" research provides new insights for promoting sustainable management of water resources and ecosystems in mountainous water source areas.
引用
收藏
页码:1469 / 1478
页数:10
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