In remote sensing, clouds appear white in the visible spectral bands primarily due to non-selective scattering.
This type of scattering occurs when the particles responsible for scattering (such as cloud droplets or fog) are much larger than the wavelength of the incident light.
Non-selective scattering affects all visible wavelengths equally,
hence all the colors of visible light (red, green, and blue) are scattered nearly uniformly.
The result is the perception of white color, which is a combination of all visible wavelengths.