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A data assimilation approach for groundwater parameter estimation under Bayesian maximum entropy framework

机译:贝叶斯最大熵框架下地下水参数估计数据同化方法

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摘要

Spatial heterogeneity in groundwater system introduces significant challenges in groundwater modeling and parameter calibration. In order to mitigate the modeling uncertainty, data assiilation methods have been applied in the parameter estimation by assessing the uncertainties from both groundwater model and observations. In practice, the observations from groundwater system can be limited, and furthermore, boundary conditions and hydrogeological parameters, such as hydraulic conductivity, can be uncertain and biased. In order to handle the uncertain observations, this study applied the Bayesian maximum entropy (BME) for a data assimilation approach that integrates groundwater model, MODFLOW, and a variety of observations with uncertainties. In BME, no distributional assumption is imposed in the uncertain observations. We conducted numerical simulation with datasets of hard data of heads and hydrogeological parameters, uncertain head data on boundary, and uncertain hydrogeological parameters, i.e., hydraulic conductivity and storage coefficient. Three numerical scenarios with differerent combinations of datasets were conducted. Results show that the proposed data assimilation approach can gradually improve the modeling performance in the sense of lower mean squared errors over time. Moreover, the inclusion of uncertain observations can further improve the efficiency and accuracy in parameter estimation and hydraulic head prediction.
机译:地下水系统中的空间异质性在地下水建模和参数校准中引入了重大挑战。为了减轻建模不确定度,通过评估地下水模型和观察的不确定性,在参数估计中应用了数据兼除方法。在实践中,地下水系统的观察可以受到限制,此外,边界条件和水力地质参数,例如液压导电性,可能是不确定和偏置的。为了处理不确定的观察,这项研究应用了贝叶斯最大熵(BME),以实现与地下水模型,MODFLOW和各种与不确定性的各种观察集成的数据同化方法。在BME中,在不确定的观察中没有施加分布假设。我们对头部和水文地质参数的硬数据数据集进行了数值模拟,边界上不确定的头数据,不确定的水电站参数,即液压导电性和储存系数。进行了三种具有不同数据集合组合的数值方案。结果表明,随着时间的推移,所提出的数据同化方法可以逐步提高较低平均平均误差的建模性能。此外,包含不确定的观察结果可以进一步提高参数估计和液压头预测中的效率和准确性。

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