Aerosol Radiative Forcing
A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Aerosols".
Deadline for manuscript submissions: closed (25 January 2023) | Viewed by 5713
Special Issue Editors
Interests: aerosol optical properties; aerosol radiative forcing; air pollution; atmospheric boundary layer physics; atmospheric chemistry
Special Issue Information
Dear Colleagues,
The aerosol radiation effect plays an important role in boundary layers. Aerosols can reduce surface solar radiation and increase the temperature in the upper layer by absorbing or backscattering solar radiation. Changes due to aerosols in the PBL temperature have led to a more stable atmospheric stratification and reduced energy transfer. Moreover, more aerosols can suppress the dispersion of pollutants, leading to further increases in aerosol concentrations in the lower PBL.
In different typical regions, there are considerable differences in the type and magnitude of aerosols due to local developments and human influence. There is a complex correlation between these compositional information and the optical and radiation properties of aerosols. Therefore, further research based on aerosol composition and radiation are needed.
Aerosols can affect solar radiation through absorption, reflection, and scattering. Northwest China is an important source of sand and dust. Dust aerosols not only affect local radiation, but also a wider range of radiations due to long-distance transmission. In addition, a large increase in local aerosols inhibits the diffusion of pollutants and leads to further increases in low-level aerosol concentrations.
There are great differences in the types and physical and chemical properties of aerosols between economically developed areas and relatively backward areas. There is a complex correlation between the chemical composition information of aerosols and the optical and radiative properties of aerosols, requiring further investigation.
Prof. Dr. Jinyuan Xin
Dr. Chongshui Gong
Guest Editors
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