Wang et al. (2026) Integrated analysis of surface water-groundwater interactions and enhanced hydrological forecasting of glacierized river in cold and arid regions
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Identification
- Journal: Applied Water Science
- Year: 2026
- Date: 2026-08-22
- Authors: Wenjun Wang, Aihua Long, Jiawen Yu, Haowei Tian, Yi Xiao, Qi Li, Yang Liu, Jingzhou Zhang, Xuan Liang, Yuanyuan Meng
- DOI: 10.1007/s13201-026-02946-3
Research Groups
Not specified in the provided text.
Short Summary
This study employs a coupled SWAT-MODFLOW model to quantify surface water-groundwater interactions and project future runoff trends in the glacierized headwater catchment of the Bortala River under CMIP6 climate scenarios.
Objective
- To clarify the relationship between surface water (SW) and groundwater (GW) interactions and predict future hydrological changes in a typical glacierized, spring-fed watershed in Northwest China.
Study Configuration
- Spatial Scale: Headwater catchment of the Bortala River, Northwest China.
- Temporal Scale: Historical period (1971–2020) and future projections (up to the end of the century).
Methodology and Data
- Models used: Coupled SWAT-MODFLOW (integrated with a glacier module), Budyko framework, and CMIP6 climate scenarios (SSP2-4.5 and SSP5-8.5).
- Data sources: Observed hydrometeorological parameters for model calibration and validation.
Main Results
- Historical SW-GW Interaction (1971–2020): Surface water was the dominant recharge source for groundwater, although it experienced a cumulative reduction of 26.7% from the initial historical value, with an average annual decline rate of 0.45%.
- Future Runoff Projections: Total watershed runoff is expected to increase by 13.6% under the SSP2-4.5 scenario and 14.2% under the SSP5-8.5 scenario.
- Runoff Inflection Point: A peak/inflection point in runoff is projected for the 2070s (± 10 years), occurring approximately 10 years earlier under the high-emission SSP5-8.5 scenario.
- Hydrological Risks: Intensified precipitation extremes are expected to trigger severe hydrological risks, particularly around the 2040s and 2070s.
Contributions
- Provides a quantitative assessment of surface water-groundwater interactions in a glacierized arid region, establishing a simulation system for decomposition and reconstruction of hydrological changes under future climate scenarios.
Funding
Not specified in the provided text.
Citation
@article{Wang2026Integrated,
author = {Wang, Wenjun and Long, Aihua and Yu, Jiawen and Tian, Haowei and Xiao, Yi and Li, Qi and Liu, Yang and Zhang, Jingzhou and Liang, Xuan and Meng, Yuanyuan},
title = {Integrated analysis of surface water-groundwater interactions and enhanced hydrological forecasting of glacierized river in cold and arid regions},
journal = {Applied Water Science},
year = {2026},
doi = {10.1007/s13201-026-02946-3},
url = {https://doi.org/10.1007/s13201-026-02946-3}
}
Original Source: https://doi.org/10.1007/s13201-026-02946-3