Light is scattered by the atmosphere. Blue light scatters more than red light, so the blue coming in goes all over the place and the red/yellow makes it straight to your eyes. It's called Rayleigh Scattering.
2007-01-12 16:17:53
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answer #1
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answered by eri 7
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Because air molecules absorb and re-emit mostly blue light, which gets scattered in all directions, leaving the other wavelengths to pass through the atmosphere relatively undisturbed.
The reason these molecules absorb blue light is the structure of their outer electron shells. Photons are absorbed when their energy (which varies with wavelength and therefore color) matches that of a transition from one electron shell to another.
2007-01-13 00:14:29
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answer #2
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answered by hznfrst 6
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The sky is blue partly because air scatters short-wavelength light in preference to longer wavelengths. Combined, these effects scatter (bend away in all directions) some short, blue light waves while allowing almost all longer, red light waves to pass straight through. When we look toward a part of the sky not near the sun, the blue color we see is blue light waves scattered down toward us from the white sunlight passing through the air overhead. Near sunrise and sunset, most of the light we see comes in nearly tangent to the Earth's surface, so that the light's path through the atmosphere is so long that much of the blue and even yellow light is scattered out, leaving the sun rays and the clouds it illuminates red.
Scattering and absorption are major causes of the attenuation of radiation by the atmosphere. Scattering varies as a function of the ratio of the particle diameter to the wavelength of the radiation. When this ratio is less than about one-tenth, Rayleigh scattering occurs in which the scattering coefficient varies inversely as the fourth power of the wavelength. At larger values of the ratio of particle diameter to wavelength, the scattering varies in a complex fashion described, for spherical particles, by the Mie theory; at a ratio of the order of 10, the laws of geometric optics begin to apply.
Why is the sky blue instead of violet?
Because of the strong wavelength dependence (inverse fourth power) of light scattering according to Raleigh's Law, one would expect that the sky would appear more violet than blue, the former having a shorter wavelength than the latter. There is a simple physiological explanation for this apparent conundrum. Simply put, the human eye cannot detect violet light in presence of light with longer wavelengths. There is a reason for this. It turns out that the human eye's high resolution color-detection system is made of proteins and chromophores (which together make up photoreceptor cells or "Cone" structures in the eye's fovea) that are sensitive to different wavelengths in the visible spectrum (400 nm–700 nm). In fact, there are three major protein-chromophore sensors that have peak sensitivities to yellowish-green (564 nm), bluish-green (534 nm), and blue-violet (420 nm) light. The brain uses the different responses of these chromophores to interpret the spectrum of the light that reaches the retina.
When one experimentally plots the sensitivity curves for the three color sensors (identified here as long (L), middle (M), and short (S) wavelength), three roughly "bell-curve" distributions are seen to overlap one another and cover the visible spectrum. We depend on this overlap for color sensing to detect the entire spectrum of visible light. For example, monochromatic violet light at 400 nm mostly stimulates the S receptors, but also slightly stimulates the L and M receptors, with the L receptor having the stronger response. This combination of stimuli is interpreted by the brain as violet. Monochromatic blue light, on the other hand, stimulates the M receptor more than the L receptor. Skylight is not monochromatic; it contains a mixture of light covering much of the spectrum. The combination of strong violet light with weaker blue and even weaker green and yellow strongly stimulates the S receptor, and stimulates the M receptor more than the L receptor. As a result, this mixture of wavelengths is perceived by the brain as blue rather than violet.
You could get more information from the link below...
2007-01-13 02:26:32
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answer #3
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answered by catzpaw 6
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because blue light scattered more that red light
because the colour blue is one of the most beautiful colour in the whole wide world
just joking about the last part of the answer
2007-01-13 01:15:08
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answer #4
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answered by prisky 1
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The sky is blue because the gases in the atmosphere absorb all the frequencies (colors) of light except blue.
2007-01-13 00:08:13
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answer #5
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answered by Dr Dave P 7
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you see the atmosphere is filled with oxygen, this crazy oxygen has a unique quality of reflicting any light with shortest wave length and the blue in VIBGEYOR of sun light has the shortest wave length of all so it is scarterd by oxygen making sky blue
2007-01-13 00:22:01
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answer #6
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answered by balajibis 1
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because of the cosmic dust acting like a prism
2007-01-13 03:36:08
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answer #7
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answered by jareck 1
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