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One of the most common questions in general science is: why does the sky appear blue? This concept is important for school exams, competitive exams and general knowledge. The explanation comes from how sunlight interacts with the atmosphere.

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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.

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For science exams, remember this simple line: “Blue light scatters the most because it has a shorter wavelength.” This is the core reason behind the blue sky. Rayleigh scattering also helps explain why distant mountains look bluish and why astronauts see a black sky in space. Since space lacks atmosphere, no scattering occurs, so the sky looks completely dark.

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