When scanning a spectral line, the intensity varies across the passband of the
filtergraph for any given setting of
.
Depending on the position of the center wavelength of the filtergraph, either the
blue or the red side of the transmission profile receives more light.
We have calulated the effect for a spectral absorption line with a Gaussian profile
of width
pm and core intensity
,
There are evident differences for the low resolution mode.
The line core PSF
resembles the PSF for a flat spectrum.
The PSF
at the blue line wing has a relatively sharp core with
extended wings while the red line wing PSF
is broader in the center
with less intense wings.
The high resolution mode PSFs are essentially the same for all positions in the
spectral line.
Pupil apodisation would not do any harm as long as the observed source was featureless. Spurious spectral features could be produced when there are fluctuations of intensity, and could be misinterpreted. In particular, structure-dependent displacements of a Fraunhofer line of a medium which is at rest relative to the observer could be interpreted as Doppler shifts. We studied the magnitude of such an error by including a sinusodial intensity variation whose period and contrast was varied into the source model. The intrinsic velocity of the modelled structure was zero. The spectra were analysed for Doppler shifts, any deviation from zero Doppler velocity was interpreted as a velocity error. It turns out that spurious Doppler signals also show sinusoidal modulation of the same period as the intensity modulation, but with a period-dependent phase relative to the intensity modulation.
Figure 9 shows the amplitude and phase variation of the velocity error
with the period of intensity modulation for an rms contrast of 15%,
corresponding to a high contrast structure such as penumbral filaments.
The dotted lines represent the phase between intensity fluctuation and
velocity error.
The velocity error in the low resolution mode approaches 25 m/s at scales
between 1 and 2 arcsec.
Brighter regions appear blueshifted at these scales, which corresponds to a phase
shift of
between intensity and velocity error.
A secondary maximum of 18 m/s at 0.25 arcsec shows the velocity error in phase with
the intensity modulation, so that brighter regions appear now redshifted.
The velocity error of the high resolution mode is less than 2 m/s for scales above
0.7 arcsec where bright regions experience blueshifts.
There is a maximum of just above 6 m/s in the presence of a spatial modulation with a
scale of 0.3 arcsec, or 250 km
on the solar surface, where bright regions experience redshifts.
Figure 10 shows the amplitude of the velocity error as a function of sinusodial modulation period and an rms contrast between 0 and 15%. Velocity errors of typical granular structures with an rms contrast of some 10% and scales between 1 and 2 arcsec are of the order of 15 m/s in the low resolution mode while they amount to less than 1 m/s in the high resolution mode. Scales at the diffraction limit with contrasts of 10% suffer from velocity errors of less than 5 m/s.
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