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2007-02-25 23:43:05 · 8 answers · asked by div_chandola 2 in Science & Mathematics Weather

8 answers

Because during a sunset all the high frequency colors have been scattered by the atmosphere (The blue's mostly thats why the sky is that color) and because at the horizons light has to travel through so much more atmosphere it strips out more and more of the high frequency and your only left with the reds and yellows of the lower spectrums.

Low frequency's going farther than high frequency's is also common in sound, think of how far you can hear bass from a car, but how close it has to be to hear the words.

2007-02-26 00:02:01 · answer #1 · answered by Anonymous · 2 0

Good question. Here is the scientific explanation. At sunrise and sunset when the white beam of sunlight must traverse through the longest length of atmosphere scattering by air molecules removes the blue light, leaving the longer wavelengths of red, orange, and yellow to pass on through creating the ruddy sunrise or sunset. It is simply due to scattering by molecules (called Rayleigh scattering) and/or aerosols (called Mie pronounced Me scattering). Hope this helps.

2007-02-26 00:38:52 · answer #2 · answered by 1ofSelby's 6 · 3 0

The sun's light is bent over the horizon and passes through the dirt and moisture particles in the atmosphere at a more oblique angle than if the sun was higher. This causes many more particles to reflect the sun's light, which produces the orange glow. The better the glow the higher concentration of pollution and or moisture.

2007-02-25 23:57:27 · answer #3 · answered by kellring 5 · 0 0

Whenever it's not completely filled with clouds, we can see that the sky is blue. As the sun rises and as it sets, it looks red. These two observations are related, as this experiment will show.

You will need the following materials:

-a flashlight
-a transparent container with flat parallel sides (a 10-liter [2½-gallon] aquarium is ideal)
-250 milliliters (1 cup) of milk

Set the container on a table where you can view it from all sides. Fill it ¾ full with water. Light the flashlight and hold it against the side of the container so its beam shines through the water. Try to see the beam as it shines through the water. You may be able to see some particles of dust floating in the water; they appear white. However, it is rather difficult to see exactly where the beam passes through the water.

Add about 60 milliliters (¼ cup) of milk to the water and stir it. Hold the flashlight to the side of the container, as before. Notice that the beam of light is now easily visible as it passes through the water. Look at the beam both from the side and from the end, where the beam shines out of the container. From the side, the beam appears slightly blue, and on the end, it appears somewhat yellow.

Add another ¼ cup of milk to the water and stir it. Now the beam of light looks even more blue from the side and more yellow, perhaps even orange, from the end.

Add the rest of the milk to the water and stir the mixture. Now the beam looks even more blue, and from the end, it looks quite orange. Furthermore, the beam seems to spread more now than it did before; it is not quite as narrow.

What causes the beam of light from the flashlight to look blue from the side and orange when viewed head on? Light usually travels in straight lines, unless it encounters the edges of some material. When the beam of a flashlight travels through air, we cannot see the beam from the side because the air is uniform, and the light from the flashlight travels in a straight line. The same is true when the beam travels through water, as in this experiment. The water is uniform, and the beam travels in a straight line. However, if there should be some dust in the air or water, then we can catch a glimpse of the beam where the light is scattered by the edges of the dust particles.

When you added milk to the water, you added many tiny particles to the water. Milk contains many tiny particles of protein and fat suspended in water. These particles scatter the light and make the beam of the flashlight visible from the side. Different colors of light are scattered by different amounts. Blue light is scattered much more than orange or red light. Because we see the scattered light from the side of the beam, and blue light is scattered more, the beam appears blue from the side. Because the orange and red light is scattered less, more orange and red light travels in a straight line from the flashlight. When you look directly into the beam of the flashlight, it looks orange or red.

What does this experiment have to do with blue sky and orange sunsets? The light you see when you look at the sky is sunlight that is scattered by particles of dust in the atmosphere. If there were no scattering, and all of the light travelled straight from the sun to the earth, the sky would look dark as it does at night. The sunlight is scattered by the dust particles in the same way as the light from the flashlight is scattered by particles in milk in this experiment. Looking at the sky is like looking at the flashlight beam from the side: you're looking at scattered light that is blue. When you look at the setting sun, it's like looking directly into the beam from the flashlight: you're seeing the light that isn't scattered, namely orange and red.

What causes the sun to appear deep orange or even red at sunset or sunrise? At sunset or sunrise, the sunlight we observe has traveled a longer path through the atmosphere than the sunlight we see at noon. Therefore, there is more scattering, and nearly all of the light direct from the sun is red..

2007-02-27 15:17:30 · answer #4 · answered by Anonymous · 0 0

the ambience scatters shorter wavelengths of sunshine at the same time as letting the longer wavelengths go by. hues are in simple terms how we see diverse wavelengths of sunshine. short wavelengths like blue and violet are scattered by the ambience, it really is why the sky is blue. at the same time as the daylight is putting (or growing to be), you're searching by a lot extra air then if it were larger. The shorter wavelengths of sunshine are all scattered away leaving the longer pink, orange, and yellow wavelengths to get to our eyes. The decrease the daylight receives, the redder it receives because of this because pink is the longest wavelength of sunshine we may be able to make sure and it receives the least scattered and passes by the ambience to our eyes.

2016-12-04 23:25:54 · answer #5 · answered by ? 4 · 0 0

BECOZ, THE SUN IS ORANGE IN COLOR DUE TO PRESENCE OF FIRE CAUSED BY EXPLOSION ON ITS SURFACE.HENCE, ITS LIGHT RAYS PASS THROUGH THE PARTICLES PRESENT IN THE SKY .THESE LIGHT RAYS ARE THEN EMTTED BY THE PARTICLES HAVING DIFFERENT WAVE LENGTH.HENCE, WHILE RISING OR SETING OF THE SUN, THE SKY APPEARS ORANGE.THE COLOR IS NOT SEEN DURING THE INTERMEDIATE TIME AS THE SUN IS COMPARATIVLEY FAR FROM THE EARTH.

2007-02-25 23:59:39 · answer #6 · answered by Z....... 2 · 0 0

garsh havnt u ever seen "the kid"??? its takin longer for the sun to go thru the atmosphere, + all of the polution we put in the air... but at least it looks good, even if its conna melt us all....

2007-02-25 23:52:52 · answer #7 · answered by Anonymous · 0 0

pl refer physics book

2007-02-26 00:24:17 · answer #8 · answered by Raffaele B 2 · 0 0

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