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Simulation of fine organic aerosols in the western Mediterranean area during the ChArMEx 2013 summer campaign

机译:在地中海西部模拟精细有机气溶胶 ChArMEx 2013夏季运动期间

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摘要

The simulation of fine organic aerosols with CTMs (Chemistry Transport Models) in the westernMediterranean basin has not been studied until recently. The ChArMEx (the Chemistry-Aerosol MediterraneanExperiment) SOP 2 (Special Observation Period 2) intensive field campaign in summer of 2013 gathered a largeand comprehensive dataset of observations allowing the study of different aspects of the Mediterranean atmosphereincluding the formation of organic aerosols (OA) in 3D models. In this study, we used the CHIMERE CTM toperform simulations for the duration of the SAFMED (Secondary Aerosol Formation in the MEDiterranean) period(July to August 2013) of this campaign. In particular, we evaluated four schemes for the simulation of OA,including the CHIMERE standard scheme, the VBS (Volatility Basis Set) standard scheme with twoparameterizations including aging of biogenic secondary OA, and a modified version of the VBS scheme whichincludes fragmentation and formation of non-volatile OA. The results for these four schemes are compared toobservations at two stations in the western Mediterranean basin, located in Cap Corse (Corsica) and Cap Es Pinar(Mallorca). These observations include OA mass concentration, PMF (positive matrix factorization) results ofdifferent OA fractions, and C observations showing the fossil or non-fossil origins of carbonaceous particles. Itis concluded that the modified VBS scheme is close to observations in all three aspects mentioned above; thestandard VBS scheme without BSOA (Biogenic Secondary Organic Aerosol) aging also has a satisfactoryperformance in simulating the mass concentration of OA, but not for the source origin analysis comparisons. Inaddition, the OA sources over the western Mediterranean basin are explored. OA shows a major biogenic origin,especially at several hundred meters height from the surface; however over the Gulf of Genoa near the surface, theanthropogenic origin is of similar importance. A general assessment of other species was performed to evaluatethe robustness of the simulations for this particular domain before evaluating OA simulation schemes. It is alsoshown that the Cap Corse site presents important orographic complexity which makes comparison between modelsimulations and observations difficult. A method was designed to estimate an orographic representativeness errorfor a list of species and yields an uncertainty of between 50–85 % for primary pollutants, and around 2–10 % forsecondary species, for these species model to observations comparisons are only little impacted by orography.
机译:直到最近,还没有研究使用CTM(化学迁移模型)在地中海西部盆地模拟精细的有机气溶胶。 2013年夏天,ChArMEx(化学-气溶胶地中海实验)SOP 2(特殊观察期2)密集野外活动收集了一个庞大而全面的观测数据集,从而可以研究地中海大气的不同方面,包括在海底形成的有机气溶胶(OA)的形成。 3D模型。在这项研究中,我们使用了CHIMERE CTM在该活动的SAFMED(中东地区气溶胶形成)期间(2013年7月至2013年8月)进行了模拟。特别是,我们评估了四种用于OA模拟的方案,包括CHIMERE标准方案,具有两个参数化的VBS(挥发性基础集)标准方案,其中包括生物继发OA的老化,以及VBS方案的修改版,其中包括碎片化和形成非易失性OA。将这四个方案的结果与位于西地中海盆地(位于科西嘉岛)和Cap Es Pinar(马洛卡)的两个地中海盆地的观测结果进行了比较。这些观察结果包括OA质量浓度,不同OA组分的PMF(正矩阵分解)结果,以及C观察结果,表明碳质颗粒的化石或非化石起源。结论是,修改后的VBS方案在上述所有三个方面都接近观察结果。没有BSOA(Biogenic Secondary Organic Aerosol)老化的标准VBS方案在模拟OA的质量浓度方面也具有令人满意的性能,但是对于源来源分析比较却没有。此外,还研究了地中海西部盆地的OA来源。 OA显示出主要的生物成因,特别是在距地表几百米的高度。然而,在热那亚湾地表附近,人为起源的重要性也相似。在评估OA仿真方案之前,对其他物种进行了总体评估,以评估该特定领域仿真的鲁棒性。还显示了Cap Corse站点存在重要的地形复杂性,这使得模型模拟和观测之间的比较变得困难。设计了一种方法来估计物种列表的地形代表性误差,并且对主要污染物产生的不确定性在50–85%之间,对于次生污染物的不确定性在2–10%之间,对于这些物种模型,观测结果的比较几乎不受地形影响。

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