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A novel method for calculating ambient aerosol liquid water contents based on measurements of a humidified nephelometer system

机译:一种基于加湿浊度仪系统的测量值来计算环境气溶胶液体含水量的新方法

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摘要

Water condensed on ambient aerosol particles plays significant roles in atmospheric environment, atmospheric chemistry and climate. So far, no instruments are available for real-time monitoring of ambient aerosol liquid water contents (ALWC). In this paper, a novel method is proposed to calculate ambient ALWC based on measurements of a three-wavelength humidified nephelometer system. A humidified nephelometer system measures aerosol light scattering coefficients and backscattering coefficients at three wavelengths under dry and different relative humidity (RH) conditions, and therefore provides measurements of light scattering enhancement factor (RH). The proposed method of calculating ALWC includes two steps. The first step is estimating total volume concentration of ambient aerosol particles in dry state (V (dry)) with a machine learning method based on measurements of the “dry” nephelometer. The estimated V (dry) agrees well with the measured V (dry). The second step is estimating the volume growth factor Vg(RH) of ambient aerosol particles due to water uptake using (RH) and Ångström exponent. The ALWC is calculated from the estimated V (dry) and Vg(RH). Uncertainty analysis of the estimated V (dry) and Vg(RH) is conducted. This research have bridged the gap between (RH) and Vg(RH). The advantage of this new method is that the ambient ALWC can be obtained using only measurements from a three-wavelength humidified nephelometer system. This method will facilitate the real-time monitoring of the ambient ALWC and help for studying roles of aerosol liquid water in atmospheric chemistry, secondary aerosol formation and climate change.
机译:冷凝在周围气溶胶颗粒上的水在大气环境,大气化学和气候中起着重要作用。到目前为止,还没有仪器可用于实时监测周围的气溶胶液态水含量(ALWC)。本文提出了一种基于三波长加湿浊度仪系统的测量值来计算环境ALWC的新方法。加湿浊度仪系统在干燥和不同的相对湿度(RH)条件下测量三种波长下的气溶胶光散射系数和反向散射系数,因此可以测量光散射增强因子(RH)。拟议的计算ALWC的方法包括两个步骤。第一步是使用基于“干式”浊度计测量值的机器学习方法估算干燥状态(V(干燥))下环境气溶胶颗粒的总体积浓度。估计的V(干)与测得的V(干)非常吻合。第二步是使用(RH)和ngström指数估算由于吸水而引起的周围气溶胶颗粒的体积增长因子Vg(RH)。 ALWC由估算的V(干)和Vg(RH)计算得出。对估计的V(干)和Vg(RH)进行不确定度分析。这项研究弥合了(RH)和Vg(RH)之间的鸿沟。这种新方法的优势在于,仅使用来自三波长加湿浊度仪系统的测量值即可获得环境ALWC。这种方法将有助于对环境ALWC的实时监测,并有助于研究液态气溶胶在大气化学,二次气溶胶形成和气候变化中的作用。

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