Light refraction is not the primary reason for the blue color of the sky; instead, Rayleigh scattering plays a crucial role. This scattering occurs due to dipole moments in atmospheric molecules, which scatter shorter wavelengths of light more intensely. The intensity of scattering is proportional to the inverse fourth power of the wavelength, leading to the perception of a blue sky by our eyes. While some argue that scattering and refraction are similar processes, they are distinct phenomena, with scattering being the dominant factor in this context. Understanding these interactions helps clarify why the sky appears blue rather than any other color.