变化环境下毛乌素沙地水循环分布式模拟与演变规律研究

Distributed simulation and evolution characteristics of water cycle in the Mu Us Sandy Land under changing environment

  • 摘要: 气候变化和人类活动对水文循环产生了显著影响,尤其是在干旱半干旱区.为探究变化环境下典型半干旱生态脆弱区毛乌素沙地水循环演变特征,利用WEP-L(water and energy transfer processes in large river basin)地表水模型和Visual MODFLOW(visual modular finite difference groundwater flow)地下水模型对毛乌素沙地水循环过程进行分布式模拟,基于白家川水文站实测月径流量和监测井地下水位数据进行模型参数率定与验证.结果表明,地表水模型率定期和验证期的模拟月径流量和实测月径流量的R2都在0.5以上,模拟的监测井地下水位和实测地下水位趋势较为一致,相关系数达到0.56以上.采用偏差校正的CMIP6多模式集合气候变化情景及当地取用水情景驱动地表水-地下水耦合模型,量化了变化环境下毛乌素沙地2021—2040年关键水循环要素变化特征.结果表明,未来情景下毛乌素沙地年降水量和年蒸散发量的平均增幅分别为8.0%和7.4%,年径流深呈现逐渐减少的趋势,2040年末地下水位相较于2021年末下降了约1 m.未来2种用水情景下区域地下水总补给量与排泄量的差值分别为−1.82亿、−0.97亿m3·a−1,地表径流总量与地表用水量的差值分别为1.83亿、2.29亿m3·a−1,地下水资源开发利用将面临更大挑战.研究成果可为毛乌素沙地区域水资源规划与管理提供科学支撑.

     

    Abstract: Climate changes and human activities have significant impact on hydrological cycles, especially in arid and semi-arid zones. To investigate evolution characteristics of hydrological cycle in typical semi-arid ecologically fragile areas such as the Mu Us Sandy Land under changing environment, WEP-L (water and energy transfer processes in large river basin) surface water model and Visual MODFLOW (visual modular finite difference groundwater flow) groundwater model are used in this study to simulate the water cycle process. Model parameters are calibrated and validated with measured monthly runoff from Baijiachuan hydrological station and groundwater level data from monitoring wells. The correlation coefficient between simulated and measured monthly runoff in the surface water model calibration period and validation period are both above 0.5. The trends of the simulated and measured groundwater levels in the monitoring wells are more consistent with each other, with a correlation coefficient of > 0.56. Bias-corrected CMIP6 multi-model ensemble climate change scenario and local water withdrawal scenario are used to drive the coupled surface water-groundwater model, to quantify characteristics of changes in key water cycle elements in the Mu Us Sandy Land under changing environments from 2021-2040. In future scenario, average increase of annual precipitation and annual evapotranspiration in the Mu Us Sandy Land are found to be 8.0% and 7.4% respectively, with depth of annual runoff in a gradual decreasing trend. Groundwater level at the end of 2040 will decrease about 1 m compared with the end of 2021. Difference between total regional groundwater recharge and discharge under the two water use scenarios in the future is −182 million m3·a−1 and −97 million m3·a−1, difference between total surface runoff and surface water use being 183 million m3·a−1 and 229 million m3·a−1. Therefore, development and utilization of groundwater resources will face greater challenges. This work will support regional water resources planning and management in the Mu Us Sandy Land.

     

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