Up: Understanding radio polarimetry
Subsections
3 Scalar self-calibration
The instability of our instruments limits the possibility of external
calibration against cosmic or man-made standards. The high dynamic ranges that are
now the norm depend entirely on self-calibration or selfcal
([Thompson et al. 1986]; [Perley et al. 1994]).
So far, selfcal has been known only in scalar form. Although it is almost
universally appplied, we have no complete and compelling theory to describe it. In
practice it shows a strong propensity to converge to a unique solution, -- provided
it is given enough data. Yet we have no formal proof of this uniqueness.
My aim now is to study matrix selfcal by approaching it as a generalisation of the
scalar variant. In doing so, the best one may expect is to reach an analogously
incomplete understanding. As we shall see, this is enough for making interesting
inferences.
I begin by reviewing scalar selfcal. I ignore the effect of noise, except to note
that it introduces an element of uncertainty into the entire process that may in
unfavourable cases subvert the apparent uniqueness of our solution. As a rule this
does not appear to happen in practice.
3.1 Scalar self-calibration
Scalar selfcal works on the basis of two assumptions:
- All instrumental effects are antenna-based, i.e. the correlator is
error-free. Thus our observed visibility is given by
- The sky is "relatively empty'': The source brightness is nonzero only in a minor
fraction of the observed field, the source's support. In practice, it turns
out that the support need not be known a priori, but can be found and successively
refined by inspection of provisional "dirty'' images.
Given a set of observations, selfcal seeks to find antenna gains
and
visibilities
that are consistent with them:
 |
|
|
(10) |
Obviously, one solution consists in the true gains and visibilities. In
addition, Eq. (10) is satisfied by the combination
 |
|
|
(11) |
for any conceivable set of multipliers
.
For each of these, the visibilities
in turn correspond to a source model B' according to Eq. (4):
 |
|
|
(12) |
If the source support is limited as assumed, the sum contains only a limited number
L of terms for which
can differ from zero. For a properly conditioned
observation, the number of visibility samples (of order MN(N-1)/2) is much greater
than that of unknowns: MN values of the
plus L values of
.
The system is now overdetermined, but we have already seen that it admits at least
one solution. It is not unique, however. Indeed, if all the
equal one value
x, Eq. (12) can be rewritten as
which defines a brightness solution
 |
|
|
(13) |
Obviously, B' is confined to the support of B. Actually it is an exact but scaled
replica.
Other solutions are unlikely to exist. If we should allow the
to take
independent values, this results in scattering of brightness away from the source to
other parts of the image. It is reasonable to conjecture that it is impossible for
any "wild'' combination of
values to produce a false brightness image that
nonetheless vanishes everywhere outside the source support. Practical experience of
two decades supports this conjecture, -- but I repeat that a formal proof is
lacking and the solution may not always be robust against the effect of noise.
The above argument pinpoints the support limitation as the agent that makes selfcal
work. This idea does not seem to have been systematically exploited before, but
Leppänen et al. (1995) advance it in discussing the construction of the polarized part
for a source model whose total intensity is already available (cf.
Sect. 7.2).
3.2 Calibration versus alignment
Equation (14)
does not represent a complete calibration: out of the infinite number
of solutions that mutually differ by their positive scale factors xx*, the
selfcal procedure arbitrarily selects one. This non-uniqueness is fundamental. On
the basis of selfcal alone, we have no way of knowing what value x has. We must
fix the brightness scale afterwards by other means.
What selfcal does achieve is to reduce all the errors
in the individual
visibility measurements to a single value x: it lines up the measurements,
forcing them all to conform to one common scale factor. As a result, extremely high
dynamic ranges can be attained even though the absolute brightness scale is unknown.
Strictly, the calibration is incomplete and we ought to replace "self-calibration''
by the more precise term "self-alignment''. The distinction is a bit academic
here, but will become crucially important when we explore matrix selfcal.
It is not immediately clear from the present discussion that the absolute sky
position is also lost in self-calibration. To establish this, one must consider the
properties of the Fourier-transform relation Eq. (12). The effect is not
directly relevant here, but it should not be forgotten.
Up: Understanding radio polarimetry
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