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Source Reconstruction of Atmospheric Releases by Bayesian Inference and the Backward Atmospheric Dispersion Model: An Application to ETEX-I Data

机译:贝叶斯推理和后向大气分散模型的大气释放源重建:etex-i数据的应用

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Source term reconstruction methods attempt to calculate the most likely source parameters of an atmospheric release given measurements, including both location and release amount. However, source term reconstruction is vulnerable to uncertainties. In this paper, a method combining Bayesian inference with the backward atmospheric dispersion model is developed for robust source term reconstruction. The backward model is used to quantify the relationship between the source and measurements and to reduce the search range of the Bayesian inference. A Markov chain Monte Carlo method is used to sample from the multidimensional parameter space of the source term. The source location and release rate are estimated simultaneously, and the posterior probability distribution is produced by applying Bayes’ theorem. The proposed method is applied to a set of real concentration data from the ETEX-I experiment. The results demonstrate that the source location is estimated to be ?2.86°?±?1.01°E, 48.25°?±?0.33°N, and the release rate is estimated to be 20.16?±?3.56?kg/h. The true source location is correctly estimated to be within a one standard deviation interval, and the release rate is correctly determined to be within a three standard deviation interval.
机译:源期限重建方法尝试计算大气释放给定测量的最可能源参数,包括位置和释放量。然而,源期限重建易受不确定性的影响。本文开发了一种与向后大气分散模型结合贝叶斯推断的方法,用于鲁棒源期限重建。向后模型用于量化源和测量之间的关系,并减少贝叶斯推断的搜索范围。 Markov Chain Monte Carlo方法用于从源期限的多维参数空间中进行采样。同时估计源位置和释放速率,并且通过应用贝叶斯定理来产生后部概率分布。所提出的方法应用于Etex-I实验的一组实浓度数据。结果表明,源位置估计为2.86°α≤1.01°E,48.25°?±0.33°N,释放速率估计为20.16?±3.56?kg / h。真正的源位置被正确地估计到一个标准偏差间隔内,并且释放速率被正确地确定为在三个标准偏差间隔内。

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