The gas molecules in the atmosphere scatter the higher-energy (high frequency) blue portion of the sunlight more than they scatter the lower-energy red portion of the sunlight
When the Sun is lower in the horizon (near sunrise or sunset), the sunlight must travel through a greater thickness of atmosphere than it does when it is overhead, and even more light is scattered (not just blue, but also green, yellow, and orange) before the light reaches your eyes. This makes the sun look much redder.
2006-10-21 16:03:17
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answer #1
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answered by Majdi B 3
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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.
2006-10-21 22:30:32
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answer #2
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answered by The Count 4
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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.
2006-10-22 00:37:59
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answer #3
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answered by Anonymous
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The Sky is blue because of the Oxygen content. oxygen is a gas that reflects blue light. It is as simple as that. Oceans also reflect blue light and absorb light in the lower frequency Infra Red area.
2006-10-21 22:34:28
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answer #4
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answered by Anonymous
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The answer from The Count is correct. That is also why the sun looks red/orange at sunrise/sunset and looks white when it is directly overhead.
2006-10-21 22:36:29
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answer #5
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answered by Darrell Keller 2
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Light is scattered off molecules in the atmosphere. Look up 'Rayleight scattering'.
It is NOT because the light is reflected off the ocean.
2006-10-21 22:28:29
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answer #6
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answered by eri 7
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Because of Raman effect.
2006-10-21 23:00:12
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answer #7
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answered by Anonymous
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I already asked that... There's some scientific reason, but I can't remember...
2006-10-21 22:34:33
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answer #8
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answered by ♥ His Truly 2
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1,088
2006-10-21 22:35:07
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answer #9
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answered by zen 7
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