The sky appears blue mainly because of a phenomenon called Rayleigh Scattering. Sunlight is made of different colours, each with different wavelengths. When sunlight enters Earth’s atmosphere, it collides with tiny gas molecules like oxygen and nitrogen. The shorter wavelengths—blue and violet—scatter much more than red or yellow. Since our eyes are more sensitive to blue light, we see the sky as blue.
This scattering effect helps explain why sunsets appear red or orange. During sunset, sunlight travels through a thicker layer of atmosphere, scattering away the blue light and letting red colours dominate. Understanding this concept is important for Physics chapters on light and atmosphere.