The offsets of the T-T plots between 408 MHz and the final 22 MHz map
are in the range 10 kK at 22 MHz. The mean of 11 offset values at
intervals of 10
in declination from +79
to -21
is -5.1 kK with an rms deviation of 11.1 kK. This mean offset
is of the same order as that derived for the T-T plot of zenith data
(see Fig. 1). From these data alone, however, it is not
possible to decide the extent of the true offsets in either the 22 MHz
or the 408 MHz data. The 408 MHz data is suspected of having offsets
as large as 2 K (Reich & Reich 1988) and may also have a
baselevel correction of 5 K. If the average spectral index between 22
and 408 MHz is 2.50, these values correspond to 2.8 kK and 7.2 kK at
22 MHz.
In this section we examine the possible effects on our data of our imperfect knowledge of the properties of the antennas. The antennas used at 22 MHz and 408 MHz are of different types, and need to be discussed separately.
If emission received in the sidelobes made a significant contribution
to antenna temperature, then errors would result. These would be
especially significant in the map of spectral index, because the
sidelobe responses of the two very different antennas would receive
emission from different parts of the sky. The greatest effect would
occur in measurements of those parts of the sky where the brightness
temperature is the lowest (around 9 hours, 30) with emission from
the bright Galactic plane being received in the far sidelobes of the
antennas. As an example of such effects, Landecker & Wielebinski
(1970),
using the Parkes 64-m telescope at 150 MHz, found that about one third
of the antenna temperature at the sky minimum arose from sidelobe
contributions.
The response of the 22 MHz antenna is, in principle, completely
calculable from the geometry of the array, and from the phasing and
grading applied to the array elements. The angular
size of the main beam proved to be very close to the calculated value.
The net sidelobe solid angle should be zero, implying a beam
efficiency of 1.0. Sidelobe responses, apart from their effects near strong
sources, should not affect the measurement of the broad structure
which is the focus of this paper. Measurements of the antenna response
using the bright sources Cas A and Cyg A (Costain et al. 1969) bear out
this expectation. The dynamic range of these measurements is about 30 dB,
determined by the ratio of the flux density of Cyg A (29 100 Jy)
to the confusion limit for the telescope (30 Jy). Sidelobes above
this level were confined to the NS and EW planes (strictly a small
circle EW, depending on the phasing in declination) and were alternately
positive and negative, as expected, and
close to the predicted amplitude. Sidelobe response fell below the
detection limit within 10 of the main beam in the EW direction
and below 1% within 18
of the main beam in the NS
plane. These measurements verify our assertion that the performance of
the telescope at the zenith is well understood (Cas A and Cyg A pass
within 10
of the zenith at DRAO).
We are confident that the response of the antenna to the extended
background was as predicted near the zenith because of the linear
relationship between the 22 and 408 MHz brightness temperatures with
the expected spectral index at that declination
(48.8). We know that the behaviour away from the zenith
departed from the expected response for the extended emission
features, but not for point sources. We tentatively attribute this
to inadequately compensated mutual impedance effects between phased
rows of dipoles in the array. At increasing zenith angles, these
effects may have dominated the predicted response of individual dipoles
above a reflecting screen.
The available measurements suggest, however, that the sidelobes of the
complete telescope (as opposed to the individual groups of radiating
elements) were still confined to the predicted regions, even at large
zenith angles. If we assume that the sidelobe level was all
positive and at the detection limit (-30 dB) in two 180 strips
in the EW and NS directions, each equal in width to the main beam,
then the beam efficiency would be 0.9, better than most reflector
antennas. However, this is very much a worst-case assumption, and it
is probably safe to conclude that the beam efficiency was
0.95. Furthermore, the largest sidelobes lie in the NS plane, and,
when the main beam is measuring the coldest region of the sky, these
sidelobes do not intersect the bright Galactic plane. We therefore
feel justified in ignoring the effects of the sidelobe response of the
22 MHz telescope.
The 408 MHz data were not directly corrected for sidelobe contributions, but an
indirect correction was applied (Haslam et al. 1982). The
absolutely calibrated survey at 404 MHz made by Pauliny-Toth & Shakeshaft
(1962) with a beam of
about 7.5 was used to establish both the zero-level and the temperature
scale of the 408 MHz survey data. Since the 404 MHz survey was corrected
for sidelobe contributions, using it as a reference for the later survey
roughly corrected those measurements for sidelobe contributions. The technique
is valid in this case since the relationship between the measured antenna
temperature and the sidelobe correction is, to a good approximation, linear.
Checks of the effectiveness of this procedure were made subsequently
by Lawson et al. (1987) and by Reich & Reich (1988)
who convolved the 408 MHz data to the broad beams of horns and other
low-sidelobe antennas used by Webster (1975) and Sironi
(1974) to measure the Galactic emission at 408 MHz. In all cases
the comparisons were satisfactory, indicating that sidelobe effects had
been effectively removed from the 408 MHz data.
Copyright The European Southern Observatory (ESO)