Satellite Optical Remote Sensing of Clouds and Aerosols: From Particle Single-Scattering and Gaseous Absorption Through Radiative Transfer to Retrieval Products

Clouds and aerosols are fundamental regulators of Earth’s radiation budget and climate system, influencing both solar and terrestrial radiation through scattering, absorption, and emission processes. Accurate characterization of their physical and radiative properties from space requires a rigorous understanding of particle single-scattering, gaseous absorption, and radiative transfer in the atmosphere, as well as reliable inversion methods. This review synthesizes the physical foundations and algorithmic implementations of satellite-based passive optical remote sensing of clouds and aerosols, spanning the ultraviolet to thermal infrared (IR) spectral range. Beginning with electromagnetic scattering theory and state-of-the-art methods for computing single-scattering by nonspherical particles and computationally efficient methods for accounting for atmospheric absorption, we discuss the radiative transfer framework underpinning cloud and aerosol retrievals. In particular, the connection between single-scattering and multiple-scattering is rigorously formulated. We then summarize operational and research-grade retrieval techniques, including cloud masking and thermodynamic phase determination, CO2slicing for cloud-top pressure, the Nakajima–King shortwave bi-spectral and IR split-window approaches for cloud optical thickness and effective particle size, inversion algorithms for determining aerosol properties from multispectral and/or multiangle radiometric and polarimetric measurements, and active-passive remote sensing synergy. Examples of the global cloud and aerosol climatologies are illustrated using observations from the Moderate Resolution Imaging Spectroradiometer (MODIS) and the Multi-Angle Imaging SpectroRadiometer (MISR). Furthermore, the unique capabilities of active remote sensing techniques using spaceborne lidar observations are briefly discussed in the context of investigating ice clouds composed of randomly and horizontally oriented ice crystals, which remain a significant challenge for conventional passive remote sensing techniques. By connecting physical theory to practical retrievals, this review highlights both the maturity of current methodologies and the remaining challenges in reducing uncertainties in particle morphology, vertical structure, absorption, and aerosol–cloud interactions. Finally, the impact of artificial intelligence (AI) on atmospheric remote sensing is briefly addressed.