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An investigation of processes controlling the evolution of the boundary layer aerosol size distribution properties at the Swedish background station Aspvreten

机译:在瑞典背景站Aspvreten上控制边界层气溶胶尺寸分布特性演变过程的研究

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Aerosol size distributions have been measured at the Swedish backgroundstation Aspvreten (58.8° N, 17.4° E). Different states of theaerosol were determined using a novel application of cluster analysis. Theanalysis resulted in eight different clusters capturing different stages ofthe aerosol lifecycle. The atmospheric aerosol size distributions wereinterpreted as belonging to fresh, intermediate and aged types of sizedistribution. With aid of back trajectory analysis we present statisticsconcerning the relation of source area and different meteorologicalparameters using a non-Lagrangian approach. Source area is argued to beimportant although not sufficient to describe the observed aerosolproperties. Especially processing by clouds and precipitation is shown to becrucial for the evolution of the aerosol size distribution. As much as60% of the observed size distributions present features that are likelyto be related to cloud processes or wet deposition. The lifetime propertiesof different sized aerosols are discussed by means of measured variabilityof the aerosol size distribution. Processing by clouds and precipitation isshown to be especially crucial in the size range 100 nm and larger. Thisindicates an approximate limit for activation in clouds to 100 nm in thistype of environment. The aerosol lifecycle is discussed. Size distributionsindicating signs of recent new particle formation (~30% of theobserved size distributions) represent the first stage in the lifecycle.Aging of the aerosol size distribution may follow two branches: eithergrowth by condensation and coagulation or processing by non-precipitatingclouds. In both cases mass is accumulated. Wet removal is the main processcapable of removing aerosol mass. Wet deposition is argued to be animportant mechanism in reaching a state where nucleation may occur (i.e.sufficiently low aerosol surface area) in environments similar to the onestudied.
机译:在瑞典背景站Aspvreten(北纬58.8°,东经17.4°)处测量了气溶胶尺寸分布。使用聚类分析的新应用确定了气溶胶的不同状态。分析导致八个不同的簇捕获了气溶胶生命周期的不同阶段。大气气溶胶的尺寸分布被解释为属于新鲜,中度和老化的尺寸分布类型。借助后向轨迹分析,我们使用非拉格朗日方法给出了有关源面积与不同气象参数之间关系的统计数据。尽管不足以描述观测到的气溶胶特性,但认为源区域很重要。尤其是通过云层和降水进行的处理对于气溶胶尺寸分布的演变至关重要。多达60%的观测到的尺寸分布呈现出可能与云过程或湿沉降有关的特征。通过测量气溶胶粒径分布的可变性来讨论不同尺寸气溶胶的寿命特性。在100 nm及更大的尺寸范围内,显示出通过云和降水进行处理尤为重要。这表明在这种类型的环境中,云中激活的近似极限为100 nm。讨论了气溶胶的生命周期。尺寸分布表明最近新的颗粒形成的迹象(约占观察到的尺寸分布的30%)代表了生命周期的第一阶段。气溶胶尺寸分布的老化可能分为两个分支:凝结和凝聚引起的增长或非沉淀云的形成。在这两种情况下,质量都是累积的。湿法去除是能够去除浮质的主要过程。据认为,在与上述类似的环境中,湿沉降是达到可能发生成核状态(即足够小的气溶胶表面积)的重要机制。

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