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中文摘要：
不同水文生态系统水循环多尺度耦合关系的研究是现代水文科学发展面临的最大挑战和长江上游为解决流域水资源问题对于水文科学最为重要的现实需求。其中由坡面水循环理论向单元集水区或小流域尺度的水循环转换认知是流域水循环与水文模拟的理论瓶颈。利用长江上游高原草地和亚高山森林水文生态分带已具有的坡面－单元集水区－小流域水文观测试验系统，构建嵌套式多尺度水循环观测试验网络，将水循环物理过程和化学过程有机结合，有选择地开展样点－坡面－单元集水区水循环多尺度对比观测试验研究，揭示不同植被覆盖下关键水循环过程不同尺度上的变化及其相互耦合关系，探索基于水与生态要素相互作用机理的水循环多尺度转换标定与推绎理论和方法，初步建立单元集水区（小流域）尺度基于尺度转换和生态－水文作用机制的水文模型，为进一步揭示长江上游典型地貌单元和生态条件下的水循环规律和水资源形成演化特征提供重要科学依据。
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期刊论文
Quantifying transpiration in a coniferous forest: Assessment of the summed components methods, sap-f
Impacts of changes in vegetation cover on soil water heat coupling in an alpine meadow of the Qingha
Spatial and temporal variability of annual and seasonal precipitation over the desert region of Chin
Water regime shifts in the active soil layer of the Qinghai-Tibet Plateau permafrost region, under d
Impacts of grassland vegetation cover on the active-layer thermal regime, northeast Qinghai-Tibet Pl
Long-term effects of revegetation on soil hydrological processes in vegetation –stabilized desert ec
Temperature effects on seasonal streamflow and variation at different spatial scales in cold regions
The influence of freeze-thaw cycles of active soil layer on surface runoff in a permafrost watershed
Stable isotopic information for Hydrological Investigation in Hailuogou Watershed on the eastern slo
Effects of changes in alpine grassland vegetation cover on hillslope hydrological processes in a per
Variability of Soil Thermal and Hydrological Dynamics and Their Relationship to Changes in Vegetatio
Influences of alpine ecosystem degradation on soil temperature in the freezing-thawing process on Qi
Response of soil heat-water processes to vegetation cover on the typical permafrost and seasonally f
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