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Vertically-resolved particle size distribution within and above the mixing layer over the Milan metropolitan area

机译:米兰都会区混合层之内和之上的垂直分辨粒径分布

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Vertical aerosol profiles were directly measured over the city of Milanduring three years (2005–2008) of field campaigns. An optical particlecounter, a portable meteorological station and a miniaturized cascadeimpactor were deployed on a tethered balloon. More than 300 verticalprofiles were measured, both in winter and summer, mainly in conditions ofclear, dry skies.The mixing height was determined from the observed vertical aerosolconcentration gradient, and from potential temperature and relative humidityprofiles. Results show that inter-consistent mixing heights can be retrievedhighlighting good correlations between particle dispersion in the atmosphereand meteorological parameters. Mixing height growth speed was calculated forboth winter and summer showing the low potential atmospheric dispersion inwinter.Aerosol number size distribution and chemical composition profiles allowedus to investigate particle behaviour along height. Aerosol measurementsshowed changes in size distribution according to mixing height. Coarseparticle profiles (dpp<1.6 μm) were, at different heights of themixing layer. The sedimentation process influenced the coarse particleprofiles, and led to a reduction in mean particle diameter for thoseparticles observed by comparing data above the mixing height with grounddata (−14.9±0.6% in winter and −10.7±1.0% in summer).Conversely, the mean particle diameter of fine particles increased above themixing height under stable atmospheric conditions; the average increase,observed by comparing data above the mixing height with ground data, was+2.1±0.1% in winter and +3.9±0.3% in summer. Ahierarchical statistical model was created to describe the changes in thesize distribution of fine particles along height. The proposed model can beused to estimate the typical vertical profile characterising launches withinpre-specified groups starting from: aerosol size and meteorologicalconditions measured at ground-level, and a mixing height estimation. Theaverage increase of fine particle diameter, estimated on the basis of themodel, was +1.9±0.5% in winter and +6.1±1.2% in summer,in keeping with experimental findings.
机译:在三年(2005-2008年)野战期间,垂直测量了整个米兰市的垂直气溶胶剖面。将光学粒子计数器,便携式气象站和小型级联撞击器部署在系留气球上。在冬季和夏季,主要在晴朗干燥的天空条件下,测量了300多个垂直剖面。 根据观察到的垂直气溶胶浓度梯度以及潜在的温度和相对湿度剖面确定了混合高度。结果表明,可以恢复相互一致的混合高度,突出显示了大气中颗粒物的散布与气象参数之间的良好相关性。计算了冬季和夏季的混合高度增长速度,表明冬季潜在的大气弥散度较低。 气溶胶数的大小分布和化学组成特征允许研究沿高度的颗粒行为。气溶胶测量表明,尺寸分布随混合高度而变化。粗粒子轮廓( d p 1.6μm)的分布与细颗粒轮廓( d p <1.6μm)处于混合层的不同高度。沉降过程影响了粗颗粒的分布,并通过将混合高度以上的数据与地面数据进行比较(冬季为-14.9±0.6%,夏季为-10.7±1.0%)观察到的那些颗粒的平均粒径减小。在稳定的大气条件下,细颗粒的平均粒径增加到超过混合高度;通过将高于混合高度的数据与地面数据进行比较,发现平均增幅在冬季为+ 2.1±0.1%,在夏季为+ 3.9±0.3%。建立了全层统计模型来描述沿高度的细颗粒尺寸分布的变化。所提出的模型可以用来估计典型的垂直剖面特征,这些特征描述了预定组内的发射,其起点是:在地面上测量的气溶胶大小和气象条件,以及混合高度估计。根据模型估计,冬季细颗粒直径的平均增长为+ 1.9±0.5%,夏季为+ 6.1±1.2%,与实验结果一致。

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