<p><strong>Abstract.</strong> Chemical composition of 39 cloud samples and droplet size distribution in 24 cloud events were investigated at the summit of Mt. Tai from July to October 2014. Inorganic ions, organic acids, metals, HCHO, H<sub>2</sub>O<sub>2</sub>, sulfur(IV), organic carbon, element carbon as well as pH and electrical conductivity were analyzed. The acidity of the cloud water significantly decreased from a reported value of pH 3.86 in 2007&#8211;2008 (Guo et al., 2012) to pH 5.87 in the present study. The concentrations of nitrate and ammonium were both increased since 2007&#8211;2008, but the overcompensation of ammonium led to the increase of the mean pH value. The microphysical properties showed that cloud droplets were smaller than 26.0&#8201;&#956;m and the most were in the range of 6.0&#8211;9.0&#8201;&#956;m. The maximum droplet number concentration (<i>N</i><sub>d</sub>) was associated with droplet sizes of 7.0&#8201;&#956;m. Cloud droplets exhibited a strong interaction with atmospheric aerosols. High PM<sub>2.5</sub> level resulted in higher concentrations of water soluble ions and smaller sizes with more numbers of cloud droplets, and further gave rise to relatively high acidity. High degrees of relative humidity facilitated the formation of large cloud droplets and led to high liquid water contents under low PM<sub>2.5</sub> level. The cloud droplets to wet deposition acted as an important sink of soluble material in the atmosphere and the dilution effect of the water content should be considered when estimating concentrations of soluble components in the cloud phase.</p>