It is assumed that the feed errors and degree of polarization are both small; authors typically state a few percent as the upper limit. It is further required that all antennas have the same type of feed. In the interferometer equation Eq. (2), second-order products of order 10-3 are dropped and errors at a few times this level are accepted.
The linearised equations can be found in Paper II (and in almost every paper on
polarimetric calibration, e.g. Thompson et al. (1986), Perley et al. (1994) and the papers quoted
in Sect. 7.2). I show them here in an elementary form for feeds with left
(L) and right (R) circularly-polarized receptors:
Usually V' is assumed to be zero. Scalar selfcal is applied to the first two lines of Eq. (19) to obtain a good I' image and complex R and L antenna-channel gains, each with an unknown phase.
In the second pair of equations, the difference between these phases enters through the g and g* factors; its effect is a polrotation in the Q,U plane of polvector space. The trailing terms in the equations describe the leakage from I to Q and U: a polconversion. As a consequence of the linearisation, polrotation and polconversion appear in a sum rather than a product.
For an unpolarized source, the leakage terms can be measured per interferometer because Q and U are zero. The Q,U-plane polrotation can only be eliminated by a measurement of some sort. Several approaches, each with their own uncertainties, are discussed in Paper II.
As with the matrix technique, unpolarized foreground or background sources can be used as in-field calibrators. An example is the observation by Wardle et al. (1998) of weak circular polarization in a quasar whose strong core is assumed to be unpolarized.
The basic idea in all these papers is to exploit the effect of parallactic-angle variations in alt-az antennas to distinguish the leakage terms in Eq. (19) from the true source visibilities. In discussing this method, I assume that the parallactic-angle rotation is corrected for beforehand: thus Eq. (19) refers to the visibities in sky coordinates and the leakage terms include the inverse of the rotation.
Cotton (1983) mentions the method without giving details.
Roberts et al. (1994) consider two types of calibrator: either an unpolarized one that may be resolved (i.e. my case of an intensity calibrator) or an unresolved one that may be polarized. In the latter case, the true Q and U visibilities in Eq. (19) are constants. The paper illustrates the difference between them and the rotating leakage terms graphically for a couple of interferometers. The leakage terms and the visibilities are well separable by a model fit, provided the parallactic angles cover a sufficiently broad range.
Leppänen et al. (1995) use the empty-sky principle of
Sects. 3.1 and 4 to separate true linear source polarization
from leakage effects: the true polarized source brightness is necessarily
confined
to the support of the total intensity, and this provides a strong constraint that the
rotated leakage terms have difficulty satisfying. A polarized-source model obeying
the constraint is used to estimate the leakage terms and the procedure can be
iterated.
The authors introduce the concept of a "leakage beam'' to characterise the transfer of brightness from total to polarized brightness. Its value at the origin represents the polconversion, its sidelobes a polconverted spatial scattering: due to the fragmented character of the quasi-scalar method, polconversion and scattering are not neatly separated and the latter is not completely suppressed. In a simulation Leppänen et al. (1995) find the leakage beam to peak at a few .1% close to the origin, in accord with the accuracy expected under quasi-scalar assumptions.
Unlike Roberts et al. (1994), these authors make no assumptions on the source. In the more comprehensive perspective of matrix theory I doubt that the information they do use is sufficient to suppress polconversion and obtain a unique solution, -- although it may be that the quasi-scalar assumptions constrain it well enough for astrophysically acceptable image fidelity.
Copyright The European Southern Observatory (ESO)