Scattering is the process by which electromagnetic radiation is redirected in different directions after interacting with particles and molecules present in the Earth's atmosphere. It is one of the most important atmospheric phenomena in remote sensing because it affects the amount and quality of solar radiation reaching the Earth's surface and the radiation reflected back to remote sensors. Scattering modifies the spectral characteristics of objects, influences image quality, and may reduce the accuracy of data interpretation. The nature and extent of scattering depend on factors such as the wavelength of the incoming radiation, the size of atmospheric particles, and the composition of the atmosphere. In remote sensing, scattering occurs when electromagnetic waves encounter gases, dust particles, water droplets, smoke, aerosols, or other suspended materials in the atmosphere. Depending on the relationship between the wavelength of radiation and the size of the atmospheric particles, scattering is classified into three main types: Rayleigh scattering, Mie scattering, and Non-selective scattering. Rayleigh scattering occurs when the atmospheric particles are