In this section we show some results of the simulations of the VLTI. These are based on ESO's optomechanical End-to-End model.
Figure16 shows the global instrumental visibility as measured by an
idealized pupil plane instrument.
The visibility measured by a true instrument will be severely effected by
thermal background at 10 m and
high spatial frequency wavefront corrugations due to the turbulent atmosphere
at the shorter wavelengths which are both not included here.
The peaks with a period of 0.5seconds in the 0.6
m visibilities
arise from the residual tracking errors of the telescopes under wind load,
which lets the two Airy disks overlap only from time to time.
These residual errors can be corrected by increasing the gain of the
fast tracking loop which has been set to low values here on purpose.
The first 100ms of each time series are dominated by the model initialization
phase and are not usable.
Residual tilt is dominating the degradation of the visibility at short wavelengths.
Figure17 shows the effect of residual tilt present in the exit
pupil plane on the resulting interferometric image for three different
wavelengths.
While for 10m the Airy disks overlap perfectly, at 2
m one can see
a slight elongation, and for 500nm the Airy disks are separated.
Another aspect that we studied is the influence of the detector when using the interferometer at low light levels. We added noise to a multiaxially combined interferogram, corresponding to 10 000 photons and 20 e- readout noise. In Fig.18 the modulus of the corresponding Fourier spectrum can be seen. The interferometric peaks which carry the signal we want to measure are blurred, thus degrading the visibility significantly.
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Figure 18:
Fourier spectrum of an image plane combined interferogram at 2![]() |
Copyright The European Southern Observatory (ESO)