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Nucleation and growth of sulfate aerosol in coal-fired power plant plumes: sensitivity to background aerosol and meteorology

机译:燃煤电厂烟羽中硫酸盐气溶胶的成核和生长:对背景气溶胶和气象学的敏感性

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摘要

New-particle formation in the plumes of coal-fired power plants and otheranthropogenic sulfur sources may be an important source of particles in theatmosphere. It remains unclear, however, how best to reproduce thisformation in global and regional aerosol models with grid-box lengths thatare 10s of kilometers and larger. The predictive power of these models isthus limited by the resultant uncertainties in aerosol size distributions.In this paper, we focus on sub-grid sulfate aerosol processes withincoal-fired power plant plumes: the sub-grid oxidation of SO withcondensation of HSO onto newly-formed and pre-existingparticles. We have developed a modeling framework with aerosol microphysicsin the System for Atmospheric Modelling (SAM), a Large-EddySimulation/Cloud-Resolving Model (LES/CRM). The model is evaluated againstaircraft observations of new-particle formation in two different power-plantplumes and reproduces the major features of the observations. We show howthe downwind plume aerosols can be greatly modified by both meteorologicaland background aerosol conditions. In general, new-particle formation andgrowth is greatly reduced during polluted conditions due to the largepre-existing aerosol surface area for HSO condensation andparticle coagulation. The new-particle formation and growth rates are also astrong function of the amount of sunlight and NO since both control OHconcentrations. The results of this study highlight the importance forimproved sub-grid particle formation schemes in regional and global aerosolmodels.
机译:燃煤电厂和其他人为硫源中羽流中的新颗粒形成可能是大气中颗粒的重要来源。然而,目前尚不清楚如何最好地在网格盒长度为10s公里或更大的全球和区域气溶胶模型中重现这种形式。因此,这些模型的预测能力受到气溶胶粒径分布不确定性的限制。在本文中,我们重点研究燃煤电厂烟气中的亚网格硫酸盐气溶胶过程:SO的亚网格氧化以及HSO冷凝成新的-形成和预先存在的粒子。我们已经在大气建模系统(SAM),大涡模拟/云解析模型(LES / CRM)中开发了具有气溶胶微物理学的建模框架。该模型针对飞机在两个不同动力源中形成新粒子的观测进行了评估,并再现了观测的主要特征。我们展示了如何通过气象和背景气溶胶条件极大地改变顺风羽状气溶胶。通常,由于HSO冷凝和颗粒凝结的气溶胶表面积大,在污染条件下,新颗粒的形成和生长会大大减少。新粒子的形成和生长速率也是日光和NO量的重要函数,因为两者均控制OH浓度。这项研究的结果强调了在区域和全球气溶胶模型中改进亚网格颗粒形成方案的重要性。

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