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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Bayesian Monte Carlo analysis applied to regional-scale inverse emission modeling for reactive trace gases
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Bayesian Monte Carlo analysis applied to regional-scale inverse emission modeling for reactive trace gases

机译:贝叶斯蒙特卡洛分析在反应性痕量气体区域尺度反演建模中的应用

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摘要

The purpose of this article is inverse modeling of emissions at regional scale for photochemical applications. The study is performed for the Ile-de-France region over a two summers (1998 and 1999) period. This area represents an ideal framework since concentrated anthropogenic emissions in the Paris region frequently lead to the formation of urban plumes. The inversion method is based on Bayesian Monte Carlo analysis applied to a regional-scale chemistry transport model, CHIMERE. This method consists in performing a large number of successive simulations with the same model but with a distinct set of model input parameters at each time. Then a posteriori weights are attributed to individual Monte Carlo simulations by comparing them with observations from the AIRPARIF network: urban NO and O_3 concentrations and rural O_3 concentrations around the Paris area. For both NO and O_3 measurements, observations used for constraining Monte Carlo simulations are additionally averaged over the time period considered for analysis. The observational constraints strongly reduce the a priori uncertainties in anthropogenic NOx and volatile organic compounds (VOC) emissions: (1) The a posteriori probability density function (pdf) for NOx emissions is not modified in its average, but the standard deviation is decreased to around 20% (40% for the a priori one). (2) VOC emissions are enhanced (+16%) in the a posteriori pdf's with a standard deviation around 30% (40% for the a priori one). Uncertainties in the simulated urban NO, urban O_3, and O_3 production within the plume are reduced by a factor of 3.2, 2.4, and 1.7, respectively.
机译:本文的目的是针对光化学应用在区域范围内对排放量进行逆向建模。这项研究是在两个夏季(1998年和1999年)期间在法兰西岛进行的。该区域是一个理想的框架,因为巴黎地区人为排放的集中经常导致城市烟羽的形成。该反演方法基于贝叶斯蒙特卡洛分析,该分析应用于区域规模的化学迁移模型CHIMERE。该方法包括使用相同的模型但每次都使用一组不同的模型输入参数执行大量连续的仿真。然后,将后验权重与AIRPARIF网络的观测值相比较,将其归因于各个Monte Carlo模拟:巴黎地区附近的城市NO和O_3浓度以及农村O_3浓度。对于NO和O_3测量,用于约束Monte Carlo模拟的观测值还要在考虑进行分析的时间段内平均。观测约束极大地减少了人为NOx和挥发性有机化合物(VOC)排放的先验不确定性:(1)NOx排放的后验概率密度函数(pdf)的平均值没有改变,但标准偏差减小到约20%(先验者为40%)。 (2)后验pdf中的VOC排放增加了(+ 16%),标准偏差在30%左右(先验者为40%)。羽流内模拟城市NO,城市O_3和O_3产量的不确定性分别降低了3.2、2.4和1.7倍。

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