We have analyzed the effects of pupil apodisation in the TESOS filtergraph on the angular resolution and accuracy of Doppler velocity measurements of solar small scale features. We confirm Beckers' observation that a telecentric mount FPI filtergraph suffers from significant pupil apodisation; even more so when also the deformation of optical phase is included in the analysis. The latter gives rise to an enhanced halo in the point spread function in the blue wing of a line when the numerical aperture is large, in comparison to calculations where the phase effects are not taken into account.
The dependence of the phase between intensity and velocity error on structure size is easy to understand. The PSF in the blue wing of a spectral line has a sharp core and broad wings compared to the PSF in the red wing where the core is broader but wings are essentially absent. A spectral line in the presence of large scale intensity fluctuations will be blurred in the blue wing because of the extended wings of the PSF and show more contrast in the red wing. The net result is an apparent blueshift in the brighter parts of the structure and an apparent redshift in the darker parts, resulting in an anti-correlation of intensity and lineshift.
In the presence of small scale intensity fluctuations, the opposite is true, because now the sharp core of the blue wing PSF wins over the broader core in the red wing, and intensity and lineshift will be correlated. Practically, there will be a mixture of scales in the observed solar structure, and the simultaneous presence of intermediate and small scales may cause correlated superposition effects which enhance the error through the phase relation. A conservative estimate of the velocity error will therefore be the sum of the peaks at intermediate and small scales. One can expect in the worst case a peak-to-valley error of 45 m/s for the low resolution mode and of 9 m/s for the high resolution mode and for a contrast of 15% rms. The error will scale linearly with the intensity contrast.
With respect to the performance of TESOS, we make the following observations:
It is conceivable that very fine structure such as small magnetic flux concentrations and umbral dots have contrasts which exceed the range that we have investigated. But even with contrasts of up to 100% the velocity error in the high resolution mode should not amount to more than 30 m/s which is still comparable to other error sources. We therefore conclude that TESOS is very well suited for high precision and high resolution investigations of the sun.
This may not be the case for other combinations of etalon characteristics and numeric
aperture in a telecetric mount filtergraph.
We have therefore calculated the Strehl ratio for the TESOS filtergraph for
magnifications corresponding to F/512 and F/64 to give an indication of the variation
with numeric aperture.
The results are shown in Fig. 11 together with the Strehl ratio of the
current magnifications.
It is evident that for a filtergraph with the spectral resolution of TESOS, the
spatial resolution is significantly affected for numerical apertures larger than
0.002, corresponding to F/250, and decays rapidly with
.
Pupil apodisation effects therefore require careful consideration in the design
of a filtergraph.
The alternative would be to use the etalons in a collimated configuration close to
a pupil.
A simple calculation shows that such a mount is not at all without problems, either.
Each surface of an etalon cavity shows deviations from a perfectly flat plane
at the scale of typically
which origin from the polishing process.
Microroughness at the level of a few nm rms adds to these deviations.
Let
be the thickness variation of the etalon's cavity as function
of position
perpendicular to the direction of propagation of light with
.
It is then easy to show from Eqs. (1) and (2) that the optical
phase
of an originally plane wavefront transmitted by the etalon
is given with
Acknowledgements
The authors wish to express their gratitude to J.M. Beckers, National Solar Observatory, for discussion and many helpful comments.
Copyright The European Southern Observatory (ESO)