Environment Research Institute, School of Environmental Science and
Engineering, Shandong University, Ji'nan, 250100, China
Shanghai Key Laboratory of Atmospheric Particle Pollution and
Prevention, Department of Environmental Science and Engineering, Institute
of Atmospheric Sciences, Fudan University, Shanghai, 200433, China
Institute for Climate and Global Change Research, School of
Atmospheric Sciences, Nanjing University, Nanjing, 210023, Jiangsu, China
Chao Zhu
Environment Research Institute, School of Environmental Science and
Engineering, Shandong University, Ji'nan, 250100, China
Environment Research Institute, School of Environmental Science and
Engineering, Shandong University, Ji'nan, 250100, China
Chengbao Li
Shanghai Key Laboratory of Atmospheric Particle Pollution and
Prevention, Department of Environmental Science and Engineering, Institute
of Atmospheric Sciences, Fudan University, Shanghai, 200433, China
Lu Liu
Environment Research Institute, School of Environmental Science and
Engineering, Shandong University, Ji'nan, 250100, China
Caihong Xu
Environment Research Institute, School of Environmental Science and
Engineering, Shandong University, Ji'nan, 250100, China
Liang Wen
Environment Research Institute, School of Environmental Science and
Engineering, Shandong University, Ji'nan, 250100, China
Likun Xue
Environment Research Institute, School of Environmental Science and
Engineering, Shandong University, Ji'nan, 250100, China
Wenxing Wang
Environment Research Institute, School of Environmental Science and
Engineering, Shandong University, Ji'nan, 250100, China
Shanghai Key Laboratory of Atmospheric Particle Pollution and
Prevention, Department of Environmental Science and Engineering, Institute
of Atmospheric Sciences, Fudan University, Shanghai, 200433, China
Leibniz Institute for Tropospheric Research (TROPOS), Atmospheric
Chemistry Department (ACD), Permoserstr. 15, 04318, Leipzig, Germany
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Cloud events at Mt. Tai were investigated for the chemical composition and size distribution of cloud droplets. An obvious rise in pH was found for elevated NH+4 during the last decade. Higher PM2.5 levels resulted in higher concentrations of water-soluble ions, smaller sizes and higher numbers of cloud droplets. The mechanism of cloud-droplet formation and the mass transfer between aerosol–gas–cloud phases were summarized to enrich the knowledge of cloud chemical and microphysical properties.
Cloud events at Mt. Tai were investigated for the chemical composition and size distribution of...
