Impact of revegetation of the Loess Plateau of China on the regional growing season water balance

被引:121
作者
Ge, Jun [1 ,2 ,3 ]
Pitman, Andrew J. [2 ,3 ]
Guo, Weidong [1 ,4 ]
Zan, Beilei [5 ,6 ]
Fu, Congbin [1 ,4 ]
机构
[1] Nanjing Univ, Inst Climate & Global Change Res, Sch Atmospher Sci, Nanjing 210023, Peoples R China
[2] Univ New South Wales, ARC Ctr Excellence Climate Extremes, Sydney, NSW 2052, Australia
[3] Univ New South Wales, Climate Change Res Ctr, Sydney, NSW 2052, Australia
[4] Nanjing Univ, Joint Int Res Lab Atmospher & Earth Syst Sci, Nanjing 210023, Peoples R China
[5] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Land Surface Proc & Climate Change Cold &, Lanzhou 730000, Peoples R China
[6] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
基金
澳大利亚研究理事会;
关键词
YELLOW-RIVER BASIN; LAND-COVER CHANGES; SOIL-MOISTURE; VEGETATION RESTORATION; INTERNAL VARIABILITY; SURFACE-TEMPERATURE; SEDIMENT LOAD; CLIMATE; MODEL; FEEDBACKS;
D O I
10.5194/hess-24-515-2020
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
To resolve a series of ecological and environmental problems over the Loess Plateau, the "Grain for Green Program" (GFGP) was initiated at the end of 1990s. Following the conversion of croplands and bare land on hill-slopes to forests, the Loess Plateau has displayed a significant greening trend, which has resulted in soil erosion being reduced. However, the GFGP has also affected the hydrology of the Loess Plateau, which has raised questions regarding whether the GFGP should be continued in the future. We investigated the impact of revegetation on the hydrology of the Loess Plateau using relatively high-resolution simulations and multiple realizations with the Weather Research and Forecasting (WRF) model. Results suggest that revegetation since the launch of the GFGP has reduced runoff and soil moisture due to enhanced evapotranspiration. Further revegetation associated with the GFGP policy is likely to further increase evapotranspiration, and thereby reduce runoff and soil moisture. The increase in evapotranspiration is associated with biophysical changes, including deeper roots that deplete deep soil moisture stores. However, despite the increase in evapotranspiration, our results show no impact on rainfall. Our study cautions against further revegetation over the Loess Plateau given the reduction in water available for agriculture and human settlements and the lack of any significant compensation from rainfall.
引用
收藏
页码:515 / 533
页数:19
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