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The formalism discussed hitherto has been called the uv-domain
Measurement Equation because it ignores image-plane effects,
i.e. instrumental effects that depend on the position in the field.
This is only valid for a dominating compact source in the centre of
the field, and then only in the case of axially symmetric systems.
Only then does the matrix , which describes effects like
primary beam and instrumental polarisation, reduce to the unit matrix.
In this section, the formalism will be generalised to the full Measurement Equation, which describes the behaviour of a real instrument observing an arbitrary brightness distribution, and thus includes image-plane effects. For k (point) sources within the primary beam, we get:
in which the matrices
(complex gain),
(leakage)
and
(nominal feed configuration) are typical uv-domain
effects in the sense that they affect all the sources in the same
way. The matrix
describes image-plane effects, which depend
on the position
in the field, and therefore
have to be applied to each source independently:
in which the sum is taken over all k sources in the field. The sums
over time t and frequency f take care of the effects of finite
integration time and bandwidth. The effects of integrating over a finite
antenna size are indistinguishable from the primary beam, and are thus
part of
(see below).
Note that the matrices
for parallactic angle and
for ionospheric Faraday rotation are now behind the sum, even though
they are (usually) the same for all sources in the field. This is
because they do not commute with
. The same is true for
tropospheric gain effects (e.g. extinction and refraction), which
should not really be lumped with the receiver gain
. It is clear that current calibration practices could do with some
critical scrutiny!
The matrix
describes the primary beam response
(including pointing errors!) of antenna i. The matrix elements are
functions of the difference vector
between the
direction vector
of the optical axis of antenna i,
and the direction vector
of a point source k,
Instrumental polarisation is an artifact caused by asymmetries in
, and thus in
.
Ionospheric Faraday rotation does not affect it, of course.
There is a growing consensus that at least two effects are involved:
the linear shape of the dipoles, which cause the familiar
`clover-leaf' patterns in Q and U, and a standing wave in the
front-end support legs. The latter effect is strongly
frequency-dependent. NB: Expressions for the elements of
for the WSRT will emerge over the summer.