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A new method for calculating number concentrations of cloud condensation nuclei based on measurements of a three-wavelength humidified nephelometer system

机译:一种新方法,用于计算云冷凝核的数量浓度基于三波长加湿浊度计系统的测量

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摘要

The number concentration of cloud condensation nuclei (CCN) plays a fundamental role in cloud physics. Instrumentations of direct measurements of CCN number concentration (N-CCN) based on chamber technology are complex and costly; thus a simple way for measuring N-CCN is needed. In this study, a new method for N-CCN calculation based on measurements of a three-wavelength humidified nephelometer system is proposed. A three-wavelength humidified nephelometer system can measure the aerosol light-scattering coefficient (sigma(sp)) at three wavelengths and the light-scattering enhancement factor (fRH). The angstrom ngstrom exponent (angstrom) inferred from sigma(sp) at three wavelengths provides information on mean predominate aerosol size, and hygroscopicity parameter (kappa) can be calculated from the combination of fRH and angstrom. Given this, a lookup table that includes sigma(sp), kappa and angstrom is established to predict N-CCN. Due to the precondition for the application, this new method is not suitable for externally mixed particles, large particles (e.g., dust and sea salt) or fresh aerosol particles. This method is validated with direct measurements of N-CCN using a CCN counter on the North China Plain. Results show that relative deviations between calculated N-CCN and measured N-CCN are within 30% and confirm the robustness of this method. This method enables simpler N-CCN measurements because the humidified nephelometer system is easily operated and stable. Compared with the method using a CCN counter, another advantage of this newly proposed method is that it can obtain N-CCN at lower supersaturations in the ambient atmosphere.
机译:云凝结核(CCN)的数量浓度在云物理学中起着基本作用。基于腔室技术的CCN数浓度(N-CCN)的直接测量仪表复杂且昂贵;因此,需要一种测量N-CCN的简单方法。在该研究中,提出了一种基于三波长加湿浊度计系统的测量的N-CCN计算的新方法。三波长加湿的浊度计系统可以在三个波长和光散射增强因子(FRH)下测量气溶胶光散射系数(SIGMA(SP))。从Sigma(SP)在三个波长下推断的埃克斯特罗姆NGStrom指数(Angstrom)提供了有关平均主要气溶胶尺寸的信息,并且可以根据FRH和Angstrom的组合来计算吸湿性参数(κ)。鉴于这一点,建立包括Sigma(SP),KAPPA和Angstrom的查找表以预测N-CCN。由于应用的前提,这种新方法不适用于外部混合颗粒,大颗粒(例如,灰尘和海盐)或新鲜气溶胶颗粒。使用华北平原上的CCN计数器,通过直接测量N-CCN进行验证。结果表明,计算的N-CCN与测量N-CCN之间的相对偏差在30%以内,确认该方法的鲁棒性。该方法可实现更简单的N-CCN测量,因为加湿的浊度计系统易于操作和稳定。与使用CCN计数器的方法相比,这种新提出的方法的另一个优点是它可以在环境大气中以较低的过饱和度获得N-CCN。

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  • 来源
    《Atmospheric Measurement Techniques》 |2018年第2期|共12页
  • 作者单位

    Jinan Univ Inst Environm &

    Climate Res Guangzhou Guangdong Peoples R China;

    Peking Univ Sch Phys Dept Atmospher &

    Ocean Sci Beijing Peoples R China;

    Jinan Univ Inst Environm &

    Climate Res Guangzhou Guangdong Peoples R China;

    Peking Univ Sch Phys Dept Atmospher &

    Ocean Sci Beijing Peoples R China;

    Peking Univ Sch Phys Dept Atmospher &

    Ocean Sci Beijing Peoples R China;

    Peking Univ Sch Phys Dept Atmospher &

    Ocean Sci Beijing Peoples R China;

    Chinese Acad Meteorol Sci State Key Lab Severe Weather Beijing Peoples R China;

    Chinese Acad Meteorol Sci State Key Lab Severe Weather Beijing Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 计量学;
  • 关键词

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