Chapter
May 16, 2024

Using Conceptual Hydrological Models for Runoff Simulation and Attribution Analysis in the Source Area of the Yellow River, China

Publication: World Environmental and Water Resources Congress 2024

ABSTRACT

The Yellow River Basin (YRB) suffers from water shortage, and the contradiction between human and water is prominent. The source area of the Yellow River (YRSA) flows through the Qinghai-Tibet Plateau, which is extremely sensitive to climate change and human activities. The annual runoff at the Tangnaihai station, the outlet section of the YRSA, accounts for around 1/3 of the total runoff in the YRB, and therefore the YRSA is an important water conservation area of the YRB. It is of great significance to carry out hydrological simulation and quantify the historical pattern and future tendency of runoff changes in the YRSA for guiding the efficient utilization of water resources and the high-quality development of the YRB. To this end, this paper constructs a research dataset from 1961 to 2017. Several experiments are conducted using the single model and combined model of IHACRES-CMD and GR4JSG, taking into account both the rainfall-runoff and snow/ice-runoff patterns. In addition, different scenarios are compared to reveal the impacts of climate change and human activities on historical runoff changes. Results show that at the Tangnaihai station, compared with the single model of IHACRES-CMD or GR4JSG, the combined model (with around 5,000 m elevation for model selection) has better simulation accuracy (calibration period: NSE = 0.80; validation period: NSE = 0.84), which is more suitable for exploring runoff changes in the YRSA. The contribution rate of climate change and human activities to the runoff changes at the Tangnaihai station is 26.7% and 73.3% for the multi-year average, 32.5% and 67.5% for the flood season, and 8.6% and 91.4% for the non-flood season, respectively.

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Go to World Environmental and Water Resources Congress 2024
World Environmental and Water Resources Congress 2024
Pages: 233 - 245

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Published online: May 16, 2024

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1State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing, China. Email: [email protected]
2State Key Laboratory of Plateau Ecology and Agriculture, School of Civil Engineering and Water Resources, Qinghai Univ., Xining, China. Email: [email protected]
Dongqin Yin [email protected]
3College of Land Science and Technology, China Agricultural Univ., Beijing, China. Email: [email protected]
4College of Land Science and Technology, China Agricultural Univ., Beijing, China. Email: [email protected]
5State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing, China. Email: [email protected]
6State Key Laboratory of Plateau Ecology and Agriculture, School of Civil Engineering and Water Resources, Qinghai Univ., Xining, China. Email: [email protected]

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