Staff Publications

Staff Publications

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    'Staff publications' is the digital repository of Wageningen University & Research

    'Staff publications' contains references to publications authored by Wageningen University staff from 1976 onward.

    Publications authored by the staff of the Research Institutes are available from 1995 onwards.

    Full text documents are added when available. The database is updated daily and currently holds about 240,000 items, of which 72,000 in open access.

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Record number 510943
Title Influences of Frozen Ground and Climate Change on Hydrological Processes in an Alpine Watershed : A Case Study in the Upstream Area of the Hei'he River, Northwest China
Author(s) Zhang, Yanlin; Cheng, Guodong; Li, Xin; Jin, Huijun; Yang, Dawen; Flerchinger, Gerald N.; Chang, Xiaoli; Bense, Victor F.; Han, Xujun; Liang, Ji
Source Permafrost and Periglacial Processes 28 (2017)2. - ISSN 1045-6740 - p. 420 - 432.
DOI https://doi.org/10.1002/ppp.1928
Department(s) Hydrology and Quantitative Water Management
WIMEK
Publication type Refereed Article in a scientific journal
Publication year 2017
Keyword(s) Climate change - Cold regions - Distributed hydrological model - Frozen ground - Hei'he River basin
Abstract

In cold regions, the occurrence of frozen ground has a fundamental control over the character of the water cycle. To investigate the impact of changing ground temperature conditions on hydrological processes in the context of climate change, a distributed hydrological model with an explicit frozen ground module was applied to an alpine watershed in the upstream area of the Hei'he River in the Qilian Mountains, northwest China. After evaluating the base model, we considered scenarios of frost-free ground and climate change. Results showed that the base model with a frozen ground module successfully captured the water balance and thermal regimes in the basin. When the frozen ground module was turned off, the simulated groundwater recharge and base flow increased by a factor of two to three because surface runoff caused by exceeding infiltration capacities at high elevations, which occurred in the base model, was eliminated. Consequently, the river hydrograph became smoother and flatter, with summer flood peaks delayed and reduced in volume. The annual mean depth where subsurface runoff was generated, was about 2.4m compared to 1.1m in the base model. For a warming climate, a combination of increasing evapotranspiration and reducing permafrost area results in smoother and flatter hydrographs, and a reduction in total river discharge. Although our analysis using numerical models has its limitations, it still provides new quantitative understanding of the influences of frozen ground and climate change on hydrological processes in an alpine watershed.

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