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Inverse modelling of the spatial distribution of NOx emissions on a continental scale using satellite data

机译:利用卫星数据对大陆尺度NOx排放的空间分布进行反演

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摘要

The recent important developments in satellite measurements of thecomposition of the lower atmosphere open the challengingperspective to use such measurements as independent information onsources and sinks of atmospheric pollutants. This study exploresthe possibility to improve estimates of gridded NOemissions used in a continental scale chemistry transport model(CTM), CHIMERE, by employing measurements performed by the GOMEand SCIAMACHY instruments. We set-up an original inverse modellingscheme that not only enables a computationally efficientoptimisation of the spatial distribution of seasonally averagedNO emissions (during summertime), but also allowsestimating uncertainties in input data and a priori emissions. Thekey features of our method are (i) replacement of the CTM by a setof empirical models describing the relationships betweentropospheric NO columns and NO emissions withsufficient accuracy, (ii) combination of satellite data fortropospheric NO columns with ground based measurements ofnear surface NO concentrations, and (iii) evaluation ofuncertainties in a posteriori emissions by means of a specialBayesian Monte-Carlo experiment which is based on random samplingof errors of both NO columns and emission rates. We haveestimated the uncertainty in a priori emissions based on the EMEPemission inventory to be about 1.9 (in terms of geometric standarddeviation) and found the uncertainty in a posteriori emissionsobtained from our inverse modelling scheme to be significantlylower (about 1.4). It is found also that a priori NOemission estimates are probable to be persistently biased in manyregions of Western Europe, and that the use of a posterioriemissions in the CTM improves the agreement between the modelledand measured data.
机译:卫星对低层大气成分的测量的最新重要进展为使用诸如大气污染物源和汇的独立信息之类的测量提供了挑战。这项研究探索了通过使用GOMEand SCIAMACHY仪器进行的测量来改善大陆规模化学迁移模型(CTM)CHIMERE中使用的网格NO排放估算的可能性。我们建立了一个原始的逆建模方案,该方案不仅可以对夏季(季节性)的季节平均NO排放量的空间分布进行高效计算优化,而且还可以估算输入数据和先验排放量的不确定性。我们方法的关键特征是(i)用一组经验模型代替CTM,该经验模型以足够的精度描述了对流层NO柱与NO排放之间的关系;(ii)对流层NO柱的卫星数据与近地面NO浓度的地面测量相结合,以及(iii)通过特殊的贝叶斯蒙特卡洛实验评估后验排放中的不确定度,该实验基于对NO柱和排放率的误差的随机采样。我们基于EMEPemission清单估算出先验排放的不确定性约为1.9(就几何标准偏差而言),发现从我们的逆建模方案获得的后验排放中的不确定性要低得多(约1.4)。还发现,在西欧许多地区,先验NO排放估算值可能会一直存在偏差,并且在CTM中使用后排放可改善建模数据与实测数据之间的一致性。

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