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Updated: Jan 18, 2026

Design and Construction of an Urban Runoff Research Facility
Published on: August 8, 2014
Climate and land use regulate vegetation-runoff interaction pathways in the three-river source region.
Guiyuan Zhang1, Darrell Tang2, Song Li3
1College of Water Resources and Architectural Engineering at Northwest Agriculture and Forestry University/Key Laboratory of Agricultural Soil and Water Engineering in Arid and Semiarid Areas at Ministry of Education, Yangling, Shaanxi, 712100, PR China; Academy of Plateau Science and Sustainability, Qinghai Normal University, Xining, 810008, PR China; Northwest A&F University ShenZhen Research Institute, Shenzhen, Guangdong, 518075, PR China.
Climate and land cover changes significantly impact alpine runoff. Vegetation growth status is a key factor mediating these effects on water resources in the Three-River Source Region.
Area of Science:
- Alpine hydrology
- Climate change impacts
- Ecosystem dynamics
Background:
- Alpine ecosystems are vital for water regulation but vulnerable to climate change.
- The Three-River Source Region (TRSR) faces altered climate and ecological conditions impacting vegetation and hydrology.
- Quantifying combined climate and ecological effects on runoff is crucial.
Purpose of the Study:
- To evaluate the relative impacts of climate, vegetation phenology, and land cover on runoff variability in the TRSR.
- To understand the mediating role of vegetation dynamics in alpine hydrological processes.
Main Methods:
- Utilized Partial Least Squares Structural Equation Modeling (PLS-SEM).
- Analyzed data from 1982 to 2018, considering temperature, precipitation, vegetation phenology, and land cover.
- Assessed direct and indirect effects on runoff variability.
Main Results:
- Vegetation growth status (GS) showed significant interannual and spatial variation, increasing annually.
- Precipitation had a strong positive direct and indirect effect on runoff.
- Temperature exhibited a strong negative direct effect, with indirect effects partially offsetting it.
- High-density forest positively influenced runoff by regulating soil moisture and evapotranspiration.
- Vegetation growth status served as a key mediator between climate and runoff.
Conclusions:
- Vegetation dynamics play a central role in alpine hydrology, modulating soil moisture and evapotranspiration.
- Understanding these interactions is vital for adaptive environmental management in alpine headwaters.
- Effective management is needed to sustain water resources and ecosystem function under changing conditions.
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