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Response of Runoff to Hydro-Meteorological Factors and Multi-Scenario Runoff Prediction in the Ganhe River Basin, Northeast China

Author

Listed:
  • Ting Wang

    (School of Hydraulic and Electric Power, Heilongjiang University, Harbin 150080, China
    School of Heilongjiang River and Lake Chief, Heilongjiang University, Harbin 150080, China)

  • Chenggang Yu

    (Heilongjiang Hydrology and Water Resources Center, Daxinganling Sub-Center, Jiagedaqi 165000, China)

  • Xinyu Wang

    (School of Hydraulic and Electric Power, Heilongjiang University, Harbin 150080, China)

  • Changlei Dai

    (School of Hydraulic and Electric Power, Heilongjiang University, Harbin 150080, China
    School of Heilongjiang River and Lake Chief, Heilongjiang University, Harbin 150080, China)

  • Zijun Wang

    (School of Hydraulic and Electric Power, Heilongjiang University, Harbin 150080, China
    School of Heilongjiang River and Lake Chief, Heilongjiang University, Harbin 150080, China
    Heilongjiang Provincial Water Investment Linhai Reservoir Water Supply Project Management Co., Ltd., Mudanjiang 157000, China)

Abstract

Hydrometeorological changes profoundly influence runoff generation and evolution in river basins. It is of great significance to carry out runoff prediction research to ensure water resources security and improve disaster prevention and mitigation capabilities. In this paper, the Ganhe River Basin in Northeast China was taken as the research object. Based on the hydrometeorological and runoff data from 1980 to 2022, a variety of statistical methods were used to systematically study the climate change, runoff evolution characteristics and driving mechanism of the basin. Combined with BP neural network model and CMIP6 climate scenario data, the future runoff changes were predicted. The results showed that the precipitation and relative humidity showed a downward trend, while the temperature, sunshine and evapotranspiration showed an upward trend during the study period. The runoff showed a non-significant upward trend, and an abrupt change occurred in 2009. After the abrupt change, the runoff increased by 38.7% compared with the baseline period. The change in land use was the most significant from 1990 to 2000, and the area of cultivated land increased significantly. Correlation analysis showed that precipitation was the dominant meteorological factor affecting runoff change, and the contribution rate of human activities was 88.51%, which was much higher than that of climate change. The BP neural network model demonstrated satisfactory simulation performance, and the training set and test set R2 reached 0.88 and 0.82, respectively. In the future, both temperature and precipitation will increase under different SSP scenarios. On this basis, the BP neural network prediction results show that the runoff of the basin is generally increasing, and the increase is the most significant under the high emission scenario, and the risk of extreme hydrological events may be further aggravated. These findings provide scientific support for water resources management and ecological conservation in the Ganhe River Basin.

Suggested Citation

  • Ting Wang & Chenggang Yu & Xinyu Wang & Changlei Dai & Zijun Wang, 2026. "Response of Runoff to Hydro-Meteorological Factors and Multi-Scenario Runoff Prediction in the Ganhe River Basin, Northeast China," Sustainability, MDPI, vol. 18(14), pages 1-38, July.
  • Handle: RePEc:gam:jsusta:v:18:y:2026:i:14:p:7043-:d:1987545
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