A clear cloudless day-time sky is blue because molecules in the air scatter blue light from the sun more than they scatter red light. When we look towards the sun at sunset, we see red and orange colours because the blue light has been scattered out and away from the line of sight.
The white light from the sun is a mixture of all colours of the rainbow. This was demonstrated by Isaac Newton, who used a prism to separate the different colours and so form a spectrum. The colours of light are distinguished by their different wavelengths. The visible part of the spectrum ranges from red light with a wavelength of about 720 nm, to violet with a wavelength of about 380 nm, with orange, yellow, green, blue and indigo between. The three different types of colour receptors in the retina of the human eye respond most strongly to red, green and blue wavelengths, giving us our colour vision.
2007-11-02 22:01:27
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answer #1
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answered by jason 4
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This question has been asked over 5000 times, and I've prepared a simple answer, without too much science:
The correct answer is that the blue light is scattered by the air molecules in the atmosphere (referred to as Rayleigh scattering). The blue wavelength is scattered more, because the scatteing effect increases with the inverse of the fourth power of the incident wavelength.
OK, but I've known science graduates who don't understand what this means.
Here's my attempt at an answer without too much physics:
I think most people know that sunlight is made up of light of several different wavelengths, and can be split up into the colours of the rainbow. Blue light has the shorter wavelength, and red the longest wavelength.
When sunlight hits the molecules in the atmosphere, the light strikes the molecules and is absorbed. The molecules vibrate and and give off, or 're-emit' the light. Because the molecules vibrate in all directions, the light is emitted in all directions (called 'scattering'). The molecules in the air are much smaller than the wavelength of visible light, but because the blue wavelength is shorter and more energetic, it reacts much more with the air molecules than the red and yellow wavelengths; which tend to pass straight through.
Because the blue radiation is re-emitted from the air molecules in all directions, it seems to us looking from the ground that the blue light is coming from everywhere; hence the sky seems blue.
Near sunset, because of the low angle of the sunlight, we see more of the red and yellow wavelength passing straight through, hence the colours of the setting sun.
BTW: The sky isn't blue because of a reflection of the sea; its the other way round, although the blue colour of the sea is mostly caused by the water molecules scattering the blue light, in a similar way. This effect is even stronger with ice; which results in the intense blue colour we see if we look down a crevasse in a glacier, or down a hole in the snow made by a ski stock..
For a complete, scientific explqanation, look up 'blue sky' in Wikipedia.
2007-11-03 04:09:31
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answer #2
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answered by AndrewG 7
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The blue color of the sky is due to Rayleigh scattering. As light moves through the atmosphere, most of the longer wavelengths pass straight through. Little of the red, orange and yellow light is affected by the air.
However, much of the shorter wavelength light is absorbed by the gas molecules. The absorbed blue light is then radiated in different directions. It gets scattered all around the sky. Whichever direction you look, some of this scattered blue light reaches you. Since you see the blue light from everywhere overhead, the sky looks blue.
As you look closer to the horizon, the sky appears much paler in color. To reach you, the scattered blue light must pass through more air. Some of it gets scattered away again in other directions. Less blue light reaches your eyes. The color of the sky near the horizon appears paler or white.
THE BLACK SKY AND WHITE SUN
On Earth, the sun appears yellow. If you were out in space, or on the moon, the sun would look white. In space, there is no atmosphere to scatter the sun's light. On Earth, some of the shorter wavelength light (the blues and violets) are removed from the direct rays of the sun by scattering. The remaining colors together appear yellow.
Also, out in space, the sky looks dark and black, instead of blue. This is because there is no atmosphere. There is no scattered light to reach your eyes.
2007-11-03 04:14:40
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answer #3
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answered by Raut N 3
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When sunlight travels through the atmosphere, blue light scatters more than the other colors, leaving a dominant yellow-orange hue to the transmitted light. The scattered light makes the sky blue; the transmitted light makes the sunset reddish orange.
2007-11-03 04:07:30
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answer #4
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answered by Alex 3
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It's only the reflection of the stratosphere. The real color of the sky is only the light prisms coming from the Sun which often reflect a whitish-blue appearance.
2007-11-03 04:06:58
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answer #5
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answered by Agent319.007 6
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Nitrogen and Oxygen molecules being penetrated by light wavelengths from the sun. If the atmosphere were methane it would also be blue. If the atmosphere were hydrochloric acid it would be yellowish red or orange, etc...
2007-11-07 00:07:29
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answer #6
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answered by Anonymous
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It is blue because the air scatters blue light. See the source below for detailed information on this
2007-11-03 04:08:07
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answer #7
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answered by DaveNCUSA 7
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...in reality it's not... what you are seeing is the water-vapor and all the other "crap" that causes a spectrum reflection of the light from the Sun creating the "blue" appearance... get up above the atmosphere (out there in space) and it's black.
2007-11-03 06:38:45
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answer #8
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answered by Anonymous
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It reflects the atmosphere. The water in the ocean is blue but sometimes it appears green, for instance.
2007-11-03 04:06:07
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answer #9
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answered by volume.10 4
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This is called Raman Effect. Sir C. V. Raman was awarded the Nobel prize for explaining this phenomenon.
2007-11-03 04:14:23
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answer #10
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answered by Atul I 2
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