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Rotation in Polarization (part 1)
The Poincaré sphere provides an abstract but useful means of
visualizing the effects of birefringence. In general, light is
elliptically polarized, meaning that the electric-field vector traces
out an ellipse as it propagates. Each point on the sphere
represents a different polarization. The blue arrow on the left
is called the
Stokes vector and points to the spot on the sphere that corresponds to
the ellipse in the upper right corner. Simple cases include
linear
polarization, represented by the equator of the sphere, and circular
polarization, given by the poles. Birefringence causes the
polarization ellipse to change as light propagates. On the
Poincaré sphere, these changes give a simple rotation of the
Stokes vector about some rotation axis. The animation shows this
effect for a rotation axis (green arrow) that lies in the equatorial
plane.
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Rotation in Polarization (part 2)
The rotation in the Stokes vector and corresponding changes in
polarization are illustrated in this animation.
A very distant galaxy produces linearly polarized light.
The light experiences birefringence on its way towards Earth.
As a result, the polarization
is different at points along its journey. When it reaches Earth, it has
a different polarization than when it was created.
We can look for this
change if we know enough about the source to determine the initial
polarization.
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Rotation in Polarization (part 3)
For many sources, there is no way of knowing what the original
polarization was, so we can't look for a direct change. However,
the effect is frequency dependent for most forms of Lorentz
violation. So, assuming that there is little frequency dependence
to begin with, any dependence in the observed polarization would
indicate birefringence and Lorentz violation. This animation
illustrates the expected frequency dependence. It begins at a low
frequency and shows how the ellipse and polarization angle change as we
move to higher frequencies.
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Annual Variations
This animation shows neutrinos produced in the Sun as one flavor
(yellow) oscillates into another flavor (violet). In this
example,
oscillations are caused by a Lorentz-violating background (red
arrows). The result is large oscillations
for neutrinos moving parallel to the field and no oscillations in
neutrinos moving perpendicular to the field. A solar-neutrino
experiment on Earth then moves through regions of large and small
oscillations, resulting in variations in the observed neutrino
flux. A
signature of this effect is then an annual variation in the number of
neutrinos of each flavor reaching Earth.
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