At the end of the day as the sun gets lower and lower on the horizon, the sun and the sky around it turn astonishing shades of red and orange, resulting in a beautiful sunset.
In this lesson, we will explain exactly why that happens, and you will never look at a sunset the same way again!
Sunsets and the Color of the Sky
If you’ve ever watched a sunset, you have no doubt seen the color of the sky slowly change from blue to shades of red, yellow, and orange.
Why does this happen? Where did all the blue light go? To understand why the sky appears a reddish shade at sunset, it is important to know about Earth’s atmosphere and how light waves interact with it.
Composition of the Atmosphere
The Earth is surrounded by an atmosphere that extends for many miles above the surface. The atmosphere has several layers, which get less dense and colder as the distance from the surface increases.Earth’s atmosphere is made up of many gas molecules.
Nitrogen and oxygen together make up most of the atmospheric gases, with nitrogen making up about 78% of the total gas in the atmosphere, and oxygen comprising about 21%. The remaining 1% contains carbon dioxide, water vapor, argon, and a few other trace gases.As light from the sun passes through the atmosphere, it interacts with these atmospheric gas molecules and this is what gives the sky its color. Before we can understand how that works, though, we need to first learn about light waves.
The Composition of Visible Light
Light from the sun appears colorless, but it actually contains ALL the colors of light mixed together.
You can see all the colors in sunlight if you let light pass through a prism. Each color of light bends a little differently as it passes from the air into the glass and back again on the other side; when light comes out of the prism, it is separated into many colors. This is the same thing that happens when you see a rainbow. Light passes through water droplets suspended in the air that act like tiny prisms, separating sunlight into many colors and creating a beautiful rainbow.
So, we now know that sunlight is made up of many colors, but have you ever thought about what light really is? This turns out to be a really difficult question that has fascinated some of the most influential scientists throughout history, including Isaac Newton and Albert Einstein. Today we know that light has properties that make it seem like both a wave and a particle.
Light travels through space as an electromagnetic wave, and when it interacts with other objects, it acts like it is made up of tiny particles called photons. Different colors of light waves have different wavelengths, with blue and purple light having the shortest wavelength (400-500 nm) and red light the longest wavelength (620-750 nm).
When light waves hit other objects, some of the photons can be absorbed and then re-emitted in a different direction.
This is known as Rayleigh scattering and is very important for giving the sky its characteristic color, both during the day and at sunrise and sunset.
As light passes through Earth’s atmosphere, it runs into the many gas molecules floating around. When this happens, some photons of light are absorbed and re-emitted in different directions.
Because of the difference in wavelength between blue and red light, it turns out that light near the blue end of the spectrum is scattered much more than light on the red end of the spectrum.During the day, the sun is more directly overhead so light passes straight through the atmosphere. Blue light is scattered in all directions while other wavelengths of light are not, so the sky appears blue during the day.
As the sun gets closer and closer to the horizon, however, it passes through the atmosphere at a greater angle and has to pass through more atmospheric gas. Blue light is still scattered more than red light, but when the sun is near the horizon, this means that the blue light is scattered away in directions that cannot be easily seen from Earth. The light passing all the way through the atmosphere is therefore rich in red, yellow, and orange colors with very little blue light left. This creates a reddish colored sunset, and the same thing happens early in the morning when the sun rises, too!
As sunlight passes through the atmosphere, light is absorbed by atmospheric gas molecules and then re-emitted in different directions, a process called Rayleigh scattering. Blue light is scattered more than red light; when light has to pass through more of the atmosphere during sunrise and sunset, most of the blue light is scattered away and only red and yellow light remain.
This makes the sunset appear red even though the sky appears blue at other times of the day.