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Grassland restoration reduces water yield in the headstream region of Yangtze River.

Identifieur interne : 000B87 ( PubMed/Curation ); précédent : 000B86; suivant : 000B88

Grassland restoration reduces water yield in the headstream region of Yangtze River.

Auteurs : Jia Li [République populaire de Chine] ; Dan Liu [République populaire de Chine] ; Tao Wang [République populaire de Chine] ; Yingnian Li [République populaire de Chine] ; Shiping Wang [République populaire de Chine] ; Yuting Yang [Australie] ; Xiaoyi Wang [République populaire de Chine] ; Hui Guo [République populaire de Chine] ; Shushi Peng [France] ; Jinzhi Ding [République populaire de Chine] ; Miaogen Shen [République populaire de Chine] ; Lei Wang [République populaire de Chine]

Source :

RBID : pubmed:28526833

Abstract

Large-scale ecological restoration programs are considered as one of the key strategies to enhance ecosystem services. The Headstream region of Yangtze River (HYZR), which is claimed to be China's Water Tower but witnessed the rapid grassland deterioration during 1970s-2000, has seen a series of grassland restoration programs since 2000. But few studies have thoroughly estimated the hydrological effect of this recent grassland restoration. Here we show that restoration significantly reduces growing-season water yield coefficient (WYC) from 0.37 ± 0.07 during 1982-1999 to 0.24 ± 0.07 during 2000-2012. Increased evapotranspiration (ET) is identified as the main driver for the observed decline in WYC. After factoring out climate change effects, vegetation restoration reduces streamflow by 9.75 ± 0.48 mm from the period 1982-1999 to the period 2000-2012, amounting to 16.4 ± 0. 80% of climatological growing-season streamflow. In contrary to water yield, restoration is conducive to soil water retention - an argument that is supported by long-term in-situ grazing exclusion experiment. Grassland restoration therefore improves local soil water conditions but undercuts gain in downstream water resources associated with precipitation increases.

DOI: 10.1038/s41598-017-02413-9
PubMed: 28526833

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<div type="abstract" xml:lang="en">Large-scale ecological restoration programs are considered as one of the key strategies to enhance ecosystem services. The Headstream region of Yangtze River (HYZR), which is claimed to be China's Water Tower but witnessed the rapid grassland deterioration during 1970s-2000, has seen a series of grassland restoration programs since 2000. But few studies have thoroughly estimated the hydrological effect of this recent grassland restoration. Here we show that restoration significantly reduces growing-season water yield coefficient (WYC) from 0.37 ± 0.07 during 1982-1999 to 0.24 ± 0.07 during 2000-2012. Increased evapotranspiration (ET) is identified as the main driver for the observed decline in WYC. After factoring out climate change effects, vegetation restoration reduces streamflow by 9.75 ± 0.48 mm from the period 1982-1999 to the period 2000-2012, amounting to 16.4 ± 0. 80% of climatological growing-season streamflow. In contrary to water yield, restoration is conducive to soil water retention - an argument that is supported by long-term in-situ grazing exclusion experiment. Grassland restoration therefore improves local soil water conditions but undercuts gain in downstream water resources associated with precipitation increases.</div>
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