Mie scattering

Mie scattering refers to the way light interacts with particles that are comparable in size to the wavelength of the light. When light hits these particles, it scatters in various directions rather than just bouncing off. This phenomenon is responsible for the bright white appearance of clouds and the blue color of the sky. Unlike Rayleigh scattering, which involves smaller particles, Mie scattering occurs with larger particles, such as dust or water droplets, leading to a more uniform scattering pattern. It plays a significant role in atmospheric optics and contributes to our visual experience of the environment.