The double slit interferometer works as follows: A plane wave which
starts in Rindler sector gets split into two partial components
which propagate through
and
. There they get modified by the
two respective scatterers. They are two pointlike dipole loops
accelerating into opposite directions. Each loop acts as a
transmitter which re-radiates the electromagnetic field from the
impinging wave. The e.m. fields emitted by these two transmitters exits through
the event horizons of
and
. Upon recombining in
they produce an interference pattern as measured on the hypersurface
of the expanding inertial observation frame. The
strength and the variations in this pattern are determined by (i) the
proper separation between the two scatterers, (ii) their relative
strengths and (iii) their relative phase. In fact, from this
interference pattern one can reconstruct the currents
and
, including the amplitudes, phases
for each of them. In brief, the expanding inertial observation
frame is the ``screen'' on which one can literally ``see'' what is
going on in each of the two accelerated frames
and
.