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Fengjing Liu

Researcher at Lincoln University (Missouri)

Publications -  33
Citations -  1312

Fengjing Liu is an academic researcher from Lincoln University (Missouri). The author has contributed to research in topics: Streamflow & Snowmelt. The author has an hindex of 17, co-authored 26 publications receiving 1137 citations. Previous affiliations of Fengjing Liu include Chinese Academy of Sciences & University of California, Merced.

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Source waters and flow paths in an alpine catchment, Colorado Front Range, United States

TL;DR: In this article, the authors used isotopic and geochemical tracers to determine the source waters and flow paths of streamflow draining high-elevation catchments of the Colorado Rocky Mountains.
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Geochemistry and source waters of rock glacier outflow, Colorado Front Range

TL;DR: In this article, the seasonal variation in the geochemical and isotopic content of the outflow of the Green Lake 5 rock glacier (RG5), located in the Green Lakes Valley of the Colorado Front Range, USA, was characterized.
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Streamflow generation in a large, alpine watershed in the southern Rocky Mountains of Colorado: Is streamflow generation simply the aggregation of hillslope runoff responses?

TL;DR: In this paper, the authors investigated the role of groundwater contributions in streamflow generation in a large alpine watershed in the southern Rocky Mountains of Colorado and found that groundwater contributions are important in stream flow generation at all scales.
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Contributions of climate and human activities to changes in runoff of the Yellow and Yangtze rivers from 1950 to 2008

TL;DR: In this article, data from eight river gauging stations and 529 meteorological stations, inside and adjacent to the study basins, were analyzed and compared to quantify the hydrological processes involved, and to evaluate the role of human activities in changing river discharges.
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Nitrate content and potential microbial signature of rock glacier outflow, Colorado Front Range

TL;DR: In this article, the nutrient content in the outflow of the Green Lake 5 rock glacier, located in the Green Lakes Valley of the Colorado Front Range, was characterized, showing that dissolved organic carbon (DOC) was present in all samples with a mean concentration of 0·85 mg L−1.