Mie scattering is best described as scattering caused by:

Mie scattering is best described as scattering that occurs when the size of particles is comparable to the wavelength of the incident light. This phenomenon is significant in understanding how light interacts with larger particles, such as water droplets, aerosols, and other atmospheric substances. Unlike Rayleigh scattering, which occurs with particles much smaller than the wavelength and primarily affects shorter wavelengths of light (like blue), Mie scattering affects all wavelengths relatively equally. As a result, it can lead to effects such as the white appearance of clouds or the visibility of light scattering in foggy conditions.

This understanding of Mie scattering is important in various applications, including remote sensing and atmospheric sciences, as it aids in predicting how light behaves when interacting with different atmospheric particles. Thus, recognizing that Mie scattering is specifically associated with particles of sizes close to the wavelength is essential for interpreting observational data and modeling atmospheric phenomena accurately.