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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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