A Modified Xinanjiang Model for Quantifying Streamflow Components in a Typical Watershed in Eastern China

混流 过程线 环境科学 水流 地表径流 水文学(农业) 分水岭 布线(电子设计自动化) 水文模型 流域 计算机科学 地质学 气候学 地理 生态学 岩土工程 生物 机器学习 地图学 计算机网络
作者
Kaibin Wu,Minpeng Hu,Yu Zhang,Jia Zhou,Dingjiang Chen
出处
期刊:Hydrology [Multidisciplinary Digital Publishing Institute]
卷期号:11 (7): 90-90 被引量:2
标识
DOI:10.3390/hydrology11070090
摘要

An accurate quantification of flow components and an understanding of water source dynamics are essential for effective water resource and quality management. However, the complexity of hydrological processes and the interference of intensive human activities pose significant challenges in precisely separating water discharge into distinct components such as surface runoff, interflow, and groundwater. The Xinanjiang (XAJ) model, a conceptual watershed hydrological model, has been developed and successfully implemented for rainfall–runoff simulations and hydrograph separations across various Chinese watersheds. While the model framework is robust, it fails to account for agricultural irrigation water withdrawals and the variations in in-stream water travel times across different hydrological regimes, introducing considerable uncertainty in simulating low-flow conditions. This study introduced modifications to the XAJ model by allowing parameter adjustments across different flow regimes and incorporating irrigation withdrawals into the runoff routing process. Utilizing a decade of hydrometeorological data (2013–2022) from the Yongan River watershed in eastern China, the modified model demonstrated improved efficiency metrics in low- and medium-flow regimes compared to the original model, with a Nash–Sutcliffe coefficient improvement from −4.43~−0.49 to 0.40~0.46, R2 from 0.21~0.36 to 0.53~0.63, and BIAS reduction from 7.60~89.08% to 2.06~12.71%. Furthermore, the modified XAJ model provided a more accurate estimation of the spatial and temporal distribution of streamflow components across sub-watersheds. The original model tended to overestimate groundwater contributions (13%) and underestimate interflow (14%), particularly in low-flow conditions. The enhanced XAJ model, thus, offers a more effective tool for identifying streamflow components, providing essential insights into hydrological processes for better management decisions.

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