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A tropospheric chemistry reanalysis for the years 2005-2012 based on an assimilation of OMI, MLS, TES, and MOPITT satellite data

机译:基于OMI,MLS,TES和MOPITT卫星数据的同化,对2005 - 2012年的对流层化学再分析

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We present the results from an 8-year tropospheric chemistry reanalysis for the period 2005-2012 obtained by assimilating multiple data sets from the OMI, MLS, TES, and MOPITT satellite instruments. The reanalysis calculation was conducted using a global chemical transport model and an ensemble Kalman filter technique that simultaneously optimises the chemical concentrations of various species and emissions of several precursors. The optimisation of both the concentration and the emission fields is an efficient method to correct the entire tropospheric profile and its year-to-year variations, and to adjust various tracers chemically linked to the species assimilated. Comparisons against independent aircraft, satellite, and ozonesonde observations demonstrate the quality of the analysed O_3, NO_2, and CO concentrations on regional and global scales and for both seasonal and yearto- year variations from the lower troposphere to the lower stratosphere. The data assimilation statistics imply persistent reduction of model error and improved representation of emission variability, but they also show that discontinuities in the availability of the measurements lead to a degradation of the reanalysis. The decrease in the number of assimilated measurements increased the ozonesonde-minus-analysis difference after 2010 and caused spurious variations in the estimated emissions. The Northern/Southern Hemisphere OH ratio was modified considerably due to the multiple-species assimilation and became closer to an observational estimate, which played an important role in propagating observational information among various chemical fields and affected the emission estimates. The consistent concentration and emission products provide unique information on year-to-year variations in the atmospheric environment.
机译:我们通过吸收来自OMI,MLS,TES和MOPITT卫星器械的多个数据集来提供8年的对流层化学再分析的结果。使用全球化学传输模型进行再分析计算,并进行集合Kalman滤波技术,同时优化各种物种的化学浓度和几种前体的排放。浓度和排放场的优化是纠正整个对流层曲线及其年度变化的有效方法,并调整与物种同化的各种示踪剂。针对独立飞机,卫星和臭氧的观察结果展示了分析的O_3,NO_2和CO浓度的质量和全球尺度以及季节性和年份的季节性和年份变异,从较低的对流层到较低的平流层。数据同化统计暗示模型误差的持续减少和改善的排放变异性表示,但他们还表明,在测量的可用性方面的不连续性导致再分析的降解。同化测量数量的减少增加了2010年后的臭氧对减去分析差异,并导致估计排放的虚假变化。由于多种物种同化,北部/南部半球OH比率被显着修改,并且更接近观察估计,这在传播各种化学领域的观测信息并影响排放估计中发挥了重要作用。一致的浓度和排放产品提供关于大气环境的年度变化的独特信息。

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