The Polarization of the Sky

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2/20/2014 The polarization of the sky http://www.polarization.com/sky/sky. html 1/2  Home Vikings Bees Rainbow History Insects Shop  Oc topus Su nglasses  Displays  Land Naked-Eye Compass Space  Riding to a Polarized Sunset The sky is polarized, as any bee will eagerly tell you. Humans (with the possible exception of the Vikings) only discovered this in 1809 thanks to Arago. Sixty years later John Tyndall demonstrated how this happens with his famous and beautiful light-shinning-through-cloudy-matter experiments [1]. Both the  polari zation and the colors of the sky are created by light "scatte ring", the technical word for light that is "bounced" in random direction s by matt er. In general, the sky is polarized tangential to a circle centered in the sun and maximum polarization is found at ninety degrees from it. Therefore, with the sun close to the zenith the sky will be polarized horizontally along the entire horizon. On the other hand, when the sun is setting West, the sky will be maximally  polari zed along the meridian and thus verti cally at the horizon due North and South. Towards the zenith just after sunse t (or before sunrise) the degree of  polari zation of the sky can reach its maxim um of about 75% in very clear days. Don't forget to test thes e facts using your polarized sungl asses next time you sunbathe on a tropical beach (a vacation-friendly non-strenuous activity). The polarization pattern of the sky can be a little more complicated than the simplest (single scattering) theory would predict. In fact, Arago himself discovered that the sky opposite to the sun is not completely unpolarized as one could expect but somewhat vertically polarized (up to 20-30% at sunset: this is sometimes given the perplexing name of negative polarization). The point where the polarization switches from vertical to horizontal going from the horizon to the zenith is called the Arago neutral point. The reason for this is that when the sun is close to (or below) the horizon its light competes with the twilight sky itself as an illumination source, or in other words, the sky at the horizon is illuminated by the rest of the sky. Two other neutral points (much more difficult to detect) are rumored to be above and below the sun (the Babinet and Brewster neutral points) [2] . Wit h the sun clo se to the zeni th the sky is pol ari zed mos tly hori zont all y. At sun set the pol ari zat ion alo ng the hori zon is mo stl y vert ica l. Why scatter can polarize light? Scatter happens because a photon excites an electron that absorbs its energy and vibrates, and this vibration re-radiates like an antenna a new photon in a random direction. The direction of the electron vibration is the same as the direction of the electric field of the incident photon. Conversely, the radiated photon has the electric field aligned with the direction of the electron vibration. Light is a transversal wave what means that the electric field "vibrates" perpendicularly to the direction of the beam. If the incident light is unpolarized, the electric field vibrates in every direction in a plane perpendicular to the beam. The electron of the scattering molecule will also vibrate confined to that plane. But if the plane is seen from the side, the vibrations appear to be confined to a line, as shown in this animation. Therefore, light scattered backwards (or forward) remains unpolarized, while light scattered at 90 degrees becomes linearly polarized (in intermediate directions it is partially polarized).  Now, it is import ant to realize that if a photon is scattered mult iple tim es instead of just once before it reaches the observer, its polari zatio n becomes random. The reason is that each scattering event is in a random 3D direction and therefore the final polarization also becomes random. Why can a polarized filter make the sky bluer? If the air were completely transparent, we would be able to see the stars during the day (nice!) but there would be no visible "sky" (not so nice). This is the same reason why you have to blow smoke on a laser beam to see it from the side. The sky tends to look sky-blue because the shorter (blue) wavelengths are more likely to be scattered than the longer (red) ones by the much smaller air molecules ("Rayleigh scattering"). Contrary to the Little Red Riding Hood tale, being dressed blue puts the photon at higher risk of interception before reaching home. But if your are looking through a lot of air (i.e. at the horizon) or when there are other larger particles (e.g. pollution) that are much more efficient scatterers than the air molecules, longer (redder) wavelengths are also likely to be scattered t owards you. At the same tim e, there is a higher chance that blue light is scattered a second time on its way to your eyes, limiting the increase of its contribution. The end result is that the sky will loose some of it color saturation and become more whitish.

Transcript of The Polarization of the Sky

8/12/2019 The Polarization of the Sky

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2/20/2014 The polarization of the sky

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  Home Vikings Bees Rainbow History Insects Shop  

O ctopus S unglasses   Displays   Land Naked-Eye Compass Space  

Riding to a Polarized Sunset

The sky is polarized, as any bee will eagerly tell you. Humans (with the possible exception of the Vikings) only discovered this in 1809 thanks to Arago. Sixty

years later John Tyndall demonstrated how this happens with his famous and beautiful light-shinning-through-cloudy-matter experiments [1]. Both the

 polarization and the colors of the sky are created by light "scattering", the technical word for light that is "bounced" in random directions by matter.

In general, the sky is polarized tangential to a circle centered in the sun and maximum polarization is found at ninety degrees from it. Therefore, with the sun

close to the zenith the sky will be polarized horizontally along the entire horizon. On the other hand, when the sun is setting West, the sky will be maximally

 polarized along the meridian and thus vertically at the horizon due North and South. Towards the zenith just after sunset (or before sunrise) the degree of 

 polarization of the sky can reach its maximum of about 75% in very clear days. Don't forget to test these facts using your polarized sunglasses next time you

sunbathe on a tropical beach (a vacation-friendly non-strenuous activity).

The polarization pattern of the sky can be a little more complicated than the simplest (single scattering) theory would predict. In fact, Arago himself discovered

that the sky opposite to the sun is not completely unpolarized as one could expect but somewhat vertically polarized (up to 20-30% at sunset: this is sometimesgiven the perplexing name of negative polarization). The point where the polarization switches from vertical to horizontal going from the horizon to the zenith is

called the Arago neutral point. The reason for this is that when the sun is close to (or below) the horizon its light competes with the twilight sky itself as an

illumination source, or in other words, the sky at the horizon is illuminated by the rest of the sky. Two other neutral points (much more difficult to detect) are

rumored to be above and below the sun (the Babinet and Brewster neutral points) [2] .

With the sun close to the zenith the sky is polarized mostly horizontally. At sunset the polarization along the horizon is mostly vertical.

Why scatter can polarize light?

Scatter happens because a photon excites an electron that absorbs its energy and vibrates, and

this vibration re-radiates like an antenna a new photon in a random direction. The direction of 

the electron vibration is the same as the direction of the electric field of the incident photon.

Conversely, the radiated photon has the electric field aligned with the direction of the electron

vibration.

Light is a transversal wave what means that the electric field "vibrates" perpendicularly to the

direction of the beam. If the incident light is unpolarized, the electric field vibrates in every

direction in a plane perpendicular to the beam. The electron of the scattering molecule will alsovibrate confined to that plane. But if the plane is seen from the side, the vibrations appear to be

confined to a line, as shown in this animation. Therefore, light scattered backwards (or 

forward) remains unpolarized, while light scattered at 90 degrees becomes linearly polarized

(in intermediate directions it is partially polarized).

 Now, it is important to realize that if a photon is scattered multiple times instead of just once before it reaches the observer, its polarization becomes random. The

reason is that each scattering event is in a random 3D direction and therefore the final polarization also becomes random.

Why can a polarized filter make the sky bluer?

If the air were completely transparent, we would be able to see the stars during the day (nice!) but there would be no visible "sky" (not so nice). This is the same

reason why you have to blow smoke on a laser beam to see it from the side. The sky tends to look sky-blue because the shorter (blue) wavelengths are more

likely to be scattered than the longer (red) ones by the much smaller air molecules ("Rayleigh scattering"). Contrary to the Little Red Riding Hood tale, being

dressed blue puts the photon at higher risk of interception before reaching home.

But if your are looking through a lot of air (i.e. at the horizon) or when there are other larger particles (e.g. pollution) that are much more efficient scatterers than

the air molecules, longer (redder) wavelengths are also likely to be scattered towards you. At the same time, there is a higher chance that blue light is scattered a

second time on its way to your eyes, limiting the increase of its contribution. The end result is that the sky will loose some of it color saturation and become more

whitish.

8/12/2019 The Polarization of the Sky

http://slidepdf.com/reader/full/the-polarization-of-the-sky 2/2