In the long-wavelength regime of the GEM experiment, there are two main sources of contamination,
aside from Galactic stray radiation, which affect invariably the antenna noise temperature of the sky.
These are the emissions of the ground and the atmosphere. The latter, being a factor of at least 20þdB
smaller than the former, can be safely considered to be an elevation-dependent contribution
to the signal level of the main beam. The ground contamination, on the other hand, requires a precise
knowledge of the spillover and diffraction sidelobes of the feed in order to discriminate its contribution
to the overall antenna noise temperature. In this section, we apply
the geometric diffraction model developed in Paper I in order to account for the
effect of shielding in the estimates of the ground signal. The shields are (see Fig. 1) a 5-m
high fence, inclined at
from the ground and standing at 6.4 m from the
pivot point of the dish, and a halo of aluminum panels extending 2.1 m from the
dish petals. The fence attenuation was estimated at the 10-dB level for 408MHz
radiation, but below 1 dB at 1465MHz.
Our analytical tools enable us to estimate, as a function of the zenith angle Z, the
amount of ground contamination due to the unshielded and diffracted components.
The estimates, in units of antenna temperature, are given according to Fresnel and
Fraunhofer diffraction theories
in order to test for near and far-field effects in the range
.
The asymmetry of the feed patterns introduces an additional complication, since
the solid angle over which the ground temperature is distributed (assumed to be
the field of view below the upper edge of the fence) is seen through a sidelobe
structure that depends on the orientation of the
-plane of the feed.
Therefore, a family of 24 profiles was prepared for each feed by rotating the
-plane in
steps around the beam axis. For a tilted dish, the
reference directions
of Fig. 7 correspond to the line of sight which clears off the edge of the halo at the smallest Z angle.
Figures 10 and 11 display the model estimates assuming a 10 dB
attenuation from the fence (as in the 408 MHz case) in the presence and
absence of the halo, respectively. Figures 12 and 13 describe the situation
of the 1465MHz channel, for which the model fence provides no significant
attenuation. The upper and lower envelopes of each family of profiles have been
identified along with some other profiles. The orientations of the 408MHz and 1465MHz
feed patterns that produce these upper and lower envelopes are indicated with
labelled arrows in Fig. 7.
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Figure:
Predicted antenna noise temperature due to transmitted and diffracted ground
radiation in the double-shielded GEM experiment at 408MHz. Two additional triple-sets of profiles
have been included to show the Fresnel and Fraunhofer estimates at 1465MHz for
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Figure: Predicted antenna noise temperature due to transmitted and diffracted ground radiation in a one-shielded (no halo) GEM experiment at 1465MHz. Legend and label explanations are as in Fig. 10. Since the assumed attenuation of the fence is small, 0.3þdB, the plotted profiles represent an effectively unshielded case |
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Figure 13: Predicted antenna noise temperature due to transmitted and diffracted ground radiation in the double-shielded GEM experiment (an effectively one-shielded, fenceless, configuration) at 1465MHz. Legend and label explanations are as in Fig. 10 |
Figures 10 through 13 characterize four types of ground contamination scenarios: (1) fence-shielded in Fig. 10, (2) double-shielded in Fig. 11, (3) unshielded in Fig. 12 and (4) halo-shielded in Fig. 13. The distinction is clear enough to show how the amount of shielding and the wavelength-dependent strength of the diffraction effects shape the ground contamination profiles. Thus, as we proceed from a weakly-diffracting and unshielded antenna scenario to a strongly-diffracting and double-shielded one, far-field diffraction effects give way to near-field ones. In doing so, the distance-dependent calculations with the Fresnel approach become more difficult to be matched by the Fraunhofer approximations, whose typical overestimating power is further increased.
Shielded scenarios produce also profiles with a tendency to resemble the underlying variation of the solid angle that exposes the ground for a given Z (see Fig. 6 in Paper I). In particular, when Z is large enough to expose unscreened ground below the fence, the corresponding profile shows a marked increase in ground signal. It should be noted that the profiles obtained with the Fraunhofer formalism in the double-shielded scenario of Fig. 10 deviate from these generalized description, since one expects the role of near-field diffraction at the longer wavelength and at the innermost shield to become significant.
The composition of the ground contamination profiles in terms of their transmitted
and diffracted components can also be investigated by analyzing the symmetrized
responses
.
The diffraction model that
we are using does not produce, however, separate estimates of transmitted and
diffracted components in the Fresnel regime. Unlike in the Fraunhofer regime,
where both components are obtained independently, the Fresnel convolution
integral for calculating the contamination by the halo (or of the dish in the
unshielded scenario) produces a transmission-embedded result. Nevertheless, in
order to obtain an equivalent form of diffraction component, we have subtracted
from the convolved result the same transmitted component as in the Fraunhofer
regime. In a very realistic sense, the definition of a spillover sidelobe reduces to
the sidelobe level that is not modified by the presence of a physical obstruction
along the line of sight of the feed and within the angular range of the ground
temperature distribution. This analytical construct allows us to plot in
Fig. 14 the ratio
of the transmitted component to the total
ground contamination in the Fresnel regime.
The reason why the unshielded scenario in Fig. 14 produces anomalous
values is a consequence of the above given definition for the spillover
component. This definition implies that the diffraction sidelobes (whose sidelobe
level is modified) can actually suppress, rather than enhance, the spillover ones.
From the point of view of a Fresnel diffraction pattern, this behavior is readily
understood as the restriction imposed by the ground temperature distribution on
the angular range spanning the relative power response of the feed. The
restriction sets effectively an upper cut-off in the amplitudes of the crests that
characterize the rippling profile of this response (see, for example, Fig. 4 in
Paper I). Thus, if the cut-off is sufficiently low the overall relative power
response can fall below unity. This spillover suppression is also present in the
other scenarios, but is not dominant and, as expected from the geometrical
argument above, it originates in the portion of the halo or dish hidden from the
outside by the structure of the fence. The effect is stronger in the absence of the
shields and it becomes more pronounced at the shorter wavelength. Similar
calculations with a relatively lower sidelobe structure also demonstrated that
in order for spillover suppression to set in, the level of the relevant sidelobes
cannot be made arbitrarily small.
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Figure:
The four ground contamination scenarios in terms of the ratio ![]() |
Although transmission dominates the ground contamination at large Z, the
curves in Fig. 14 indicate that diffraction becomes the dominant
component at lower Z as the amount of shielding is also increased. We can
quantify the relevance of the spillover sidelobes by introducing a transmission
factor
(the normalized integral under the
curves).
Accordingly, a thoroughly spillover-dominated scenario would result in
,
whereas a fully diffraction-dominated case would yield
.
Table 2 lists the transmission factor in the four shielding
scenarios analyzed in this section. Only the double-shielded scenario may be
recognized to be dominated by the diffraction sidelobes.
Finally, it should be stressed that the estimates given in this section have assumed from the start that the ground temperature distribution is an isotropic field of radiation regardless of the horizon profile. As we saw in Sect. 2 this assumption is a valid one for a contaminating signal free of horizon-dependent variations, i.e. for a truly effective double-shielded scenario. Although possible, but not desirable for experimental reasons (horizontally striped maps), the convolution of the beam pattern with an anisotropic ground temperature distribution would yield a more realistic estimate in the other three scenarios. In these cases, a set of profiles like the ones shown in Figs. 10, 12 and 13 would have to be assembled for each particular azimuth.
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