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New trajectory-driven aerosol and chemical process model Chemical and Aerosol Lagrangian Model (CALM)

机译:新的轨迹驱动气溶胶和化学过程模型化学和气溶胶拉格朗日模型(CALM)

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摘要

A new Chemical and Aerosol Lagrangian Model (CALM) has been developed andtested. The model incorporates all central aerosol dynamical processes, fromnucleation, condensation, coagulation and deposition to cloud formation andin-cloud processing. The model is tested and evaluated against observationsperformed at the SMEAR II station located at Hyyti?l?(61° 51' N, 24° 17' E) over a time period of twoyears, 2000–2001. The model shows good agreement with measurementsthroughout most of the year, but fails in reproducing the aerosol propertiesduring the winter season, resulting in poor agreement between model andmeasurements especially during December–January. Nevertheless, through therest of the year both trends and magnitude of modal concentrations show goodagreement with observation, as do the monthly average size distributionproperties. The model is also shown to capture individual nucleation eventsto a certain degree. This indicates that nucleation largely is controlled bythe availability of nucleating material (as prescribed by the[H2SO4]), availability of condensing material (in this model 15%of primary reactions of monoterpenes (MT) are assumed to produce low volatilespecies) and the properties of the size distribution (more specifically, thecondensation sink). This is further demonstrated by the fact that the modelcaptures the annual trend in nuclei mode concentration. The model is alsoused, alongside sensitivity tests, to examine which processes dominate theaerosol size distribution physical properties. It is shown, in agreement withprevious studies, that nucleation governs the number concentration duringtransport from clean areas. It is also shown that primary number emissionsalmost exclusively govern the CN concentration when air from Central Europeis advected north over Scandinavia. We also show that biogenic emissions havea large influence on the amount of potential CCN observed over the borealregion, as shown by the agreement between observations and modeled resultsfor the receptor SMEAR II, Hyyti?l?, during the studiedperiod.
机译:已经开发并测试了新的化学和气溶胶拉格朗日模型(CALM)。该模型结合了所有核心气溶胶动力学过程,从成核,凝结,凝结和沉积到云的形成和云中的处理。在2000年至2001年的两年中,对照在Hyyti?l(61°51'N,24°17'E)的SMEAR II站进行的观测对模型进行了测试和评估。该模型在整个一年的大部分时间内都与测量值显示出良好的一致性,但是在冬季期间无法再现气溶胶特性,从而导致模型与测量值之间的一致性差,尤其是在12月至1月期间。然而,在今年余下的时间里,模式浓度的趋势和幅度都与观测值一致,月平均粒径分布特性也是如此。该模型还显示可以在一定程度上捕获单个成核事件。这表明成核在很大程度上受成核物质(如[H 2 SO 4 ]规定)的可用性,凝结物质的可用性(在此模型中为15%假定单萜(MT)的一次反应可产生低挥发性物种)和尺寸分布的特性(更具体地讲,是冷凝沉)。该模型捕获了核模态浓度的年度趋势,这一事实进一步证明了这一点。该模型还与敏感性测试一起用于检查哪些过程控制着气溶胶尺寸分布的物理特性。与先前的研究一致表明,成核作用控制着从清洁区域运输过程中的数量浓度。还显示,当来自中欧的空气向北流到斯堪的纳维亚半岛时,主要排放物几乎完全由CN浓度决定。我们还表明,在研究期间,与受体SMEAR II Hyyti?l的观测结果和模拟结果之间的一致性表明,生物排放对北部地区观察到的潜在CCN量有很大影响。

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