I. Introduction
Atmospheric aerosols play an important role in the Earth’s climate and environment by directly or indirectly influencing the Earth’s radiation budget through complex interactions with solar radiation, clouds, and the atmosphere [1], [2], [3], [4], [5]. Due to the complexity of aerosol particle types and their diverse sources, the distribution of their quantity and composition on regional and global scales is very heterogeneous, with drastic spatial and temporal variations [6], which brings great uncertainties to related studies. Therefore, high-precision global aerosol inversion is a fundamental requirement for monitoring the impact of aerosols on climate, environment, and air quality.