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Assessing the impacts of climate and land use land cover changes on hydrological droughts in the Yellow River Basin using SWAT model with time-varying parameters

机译:评估气候和土地利用土地覆盖的影响,使用SWAT模型与时变参数的黄河流域水文干旱的影响

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Climate and land use land cover (LULC) are two important factors for changes in hydrological droughts in the Yellow River Basin (YRB). Quantifying their impacts on hydro-logical droughts is of great importance for drought prevention and mitigation. To better characterize hydrological droughts, we proposed a new drought index named Standard Surface water and Groundwater Index (SSGI) that considers both surface water and groundwater conditions as well as their connections using copulas. The SWAT model is used and a time-varying parameters approach is adopted to improve model simulation accuracy during different periods with significant changes in land surface characteristics due to human activities. The impacts of climate and LULC changes on hydrological droughts were then quantified. Results indicate the following: 1) time-varying parameter is not only effective but also necessary to ensure the validity of the model when dealing with significant changes in physical environment, while model parameters obtained from the baseline period calibration can degrade model performance during other periods, especially in the middle and downstream of the YRB due to LULC changes; 2) hydrological droughts became increasingly serious during the last few decades, especially in part of the basin located in the Loess Plateau areas where the ecosystem is extremely fragile; 3) climate and LULC changes have both contributed to the changes in hydrological droughts but their contributions can vary significantly spatially.
机译:气候和土地利用陆地覆盖(LULC)是黄河流域水文干旱变化的两个重要因素(YRB)。量化它们对水力逻辑干旱的影响对于干旱预防和缓解具有重要意义。为了更好地表征水文干旱,我们提出了一种名为标准地表水和地下水指数(SSGI)的新的干旱指数,其考虑了地表水和地下水条件以及使用Copulas的连接。使用SWAT模型并采用时变参数方法来改善不同时期的模型模拟精度,由于人类活动导致的土地表面特征的显着变化。然后量化了气候和LULC对水文干旱变化的影响。结果表明以下内容:1)时变参数不仅有效,而且还必须在处理物理环境中的显着变化时确保模型的有效性,而从基线周期校准获得的模型参数可能会在其他时段中降低模型性能,特别是由于LULC变化,在YRB的中下游; 2)在过去几十年中,水文干旱变得越来越严重,特别是位于生态系统非常脆弱的黄土高原地区的盆地的一部分; 3)气候和LULC变化对水文干旱的变化有贡献,但它们的贡献可能会在空间显着变化。

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