Evaluating the eco-hydrologic impacts of reforestation in the Loess Plateau, China, using an eco-hydrologic model

被引:14
作者
Peng, Hui [1 ,2 ,3 ]
Tague, Christina [2 ]
Jia, Yangwen [3 ]
机构
[1] Ocean Univ China, Minist Educ, Key Lab Marine Environm & Ecol, Qingdao, Peoples R China
[2] Univ Calif Santa Barbara, Donald Bren Sch Environm Sci & Management, Santa Barbara, CA 93106 USA
[3] China Inst Water Resources & Hydropower Res IWHR, State Key Lab Simulat & Regulat River Basin Water, Beijing, Peoples R China
基金
中国国家自然科学基金;
关键词
reforestation; the Loess Plateau; hydrological response; soil moisture; vegetation growth; FOREST ECOSYSTEM PROCESSES; WATER YIELD REDUCTION; CLIMATE VARIABILITY; INTERANNUAL VARIATION; VEGETATION CHANGES; GENERALIZED-MODEL; SOIL-WATER; CONSERVATION; CATCHMENT; CARBON;
D O I
10.1002/eco.1652
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Since the 1950s, reforestation has been widely applied in the Loess Plateau in China as a soil and water conservation measure. We examine the eco-hydrologic responses to reforestation in two neighbouring catchments in the Loess Plateau using Regional Hydro-Ecologic Simulation System. We use limited observed streamflow and other eco-hydrologic data to support and evaluate the model implementation and then apply the model to disentangle the relative roles played by inter-annual variation and longer-term trends in climate drivers and re-growth following reforestation. Our model-based analysis of trends in forest water use highlights the differences in the response of control and reforested catchments to similar declines in annual precipitation in this region over the past decades. Model estimates show that while reforestation does increase vegetation water use, the impacts on streamflow are small relative to the impact of precipitation trends on streamflow, and forest water use. Results illustrate how catchment differences in response to climate trends can confound interpretation of observed streamflow patterns in a paired catchment setting. Results also show that the greatest impact of reforestation is likely to be on groundwater recharge but also suggest that evaporation rather than transpiration is a significant contributor to hydrologic change. We also examine how declining trends in precipitation impact forest productivity. While the impact of historical precipitation declines on forest primary productivity is probably minor, model estimates suggest that forests are nearing a threshold above which further declines in precipitation will lead to more ecologically significant responses. Copyright (C) 2015 John Wiley & Sons, Ltd.
引用
收藏
页码:498 / 513
页数:16
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