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Next Section: Final Comments Title/Abstract Page: Driftscan Surveys in the Previous Section: The technique | Contents Page: Volume 14, Number 1 |
Faint periodic fluctuations in the background noise are visible in the low velocity ranges of each strip in Figure 2. These are commonly called ``standing waves'' by radio spectroscopists. In these Nançay data, they occur in the correlator quadrants that have strong Galactic HI emission, but not in the higher velocity quadrants. The standing waves arise because Galactic HI signal enters the receiving system by two paths of different length. In an ideal telescope this would not happen, but it is common in the present design of radio telescopes, since radiation entering the radio receiver may have been weakly scattered by structure that crosses the telescope's aperture; this additional scattering can deflect off-axis radiation into the beam of the telescope. When two copies of a signal take different paths to the receiver, the signal taking the longer path suffers a delay, and when the autocorrelation function is computed in the spectrometer, a correlation spike is obtained in the delay channel corresponding to the extra path length. In the Fourier transformation of the ACF to obtain the power spectrum, a single-channel spike transforms to a sinusoidal variation across the band. Thus, the path delay corresponds directly to the number of cycles of standing wave across the spectral band. For the high velocity ranges of Figure 2, there is no interfering signal entering the system with a time delay and with sufficient strength to generate standing waves, and therefore the noise characteristics in this redshift range are better behaved.

Figure 3: Schematic of multipath scattering at the Arecibo Telescope.
Representative off-axis rays, R1, R2, and R3, are seen traversing
paths of different length before arriving at the Arecibo line feed F.
In this diagram, R1 takes a direct path to the feed, while R2 and R3
are scattered from different points (S2 and S3)
on the support structure. Radiation
is actually scattered in many directions
at the scattering points S2 and S3,
but those rays that are scattered downward parallel to the incoming
on-axis rays are directed to be optimally reflected from the main
reflector directly toward the feed.
Any broadband signal entering the receiving system in multiple copies with different delays can give rise to these multipath effects. A strong source of such radiation is the Sun during daytime observations, but terrestrially generated broadband RFI, Galactic emission, strong radio continuum sources and spillover can also do it. The standing waves are often dominated by a single periodicity, representing, for example, a round trip delay between the feed cabin and the dish surface. However, a further complication is that antenna structures are often sufficiently complex that several scatterering locations can contribute (as illustrated for the Arecibo Telescope in Figure 3), producing signals in several delay channels of the ACF. When the Fourier transform is computed, the spectral passband produced by the combination of multiple sinusoidal components can be very complicated. Figure 4 illustrates the complexity of standing wave patterns caused by the Sun in some Arecibo observations made during a late afternoon observation. Note that while the feed was positioned at the same antenna coordinates, this same pattern repeated on successive (solar) days. There was a slow change in the pattern after several days as the Sun moved in declination.

Figure 4: Arecibo daytime standing waves.
Left. The data image for a single circular polarization
after the standard calibration and continuum removal.
The image contains 1250 seven second time steps for a duration of
2.4 hours. The bright, spatially resolved
galaxy M94 can be seen midway through the image in the low velocity
range. There is a faint linear feature running vertically in the image
at slightly lower velocity - this is Galactic HI emission that is aliased
into the spectrum through the baseband filters.
Right. Harmonic content of each row in the image for first
63 harmonics. The amplitudes have been averaged by 4 time steps in this
image.
As well as varying in amplitude, standing waves can drift
in phase with time, causing them to fail to subtract exactly when the simpler
forms of passband calibration are applied. This is true of the
processing that has been done to obtain Figure 2, and
substantial residuals remain in the low velocity range. There is a
time range in the observations shown in Figure 4 where the
drift is so rapid that the wave moves by a full turn of phase in just a few
minutes.
Fortunately, there is a straightforward way to
tackle this problem and remove even these complicated patterns from
the driftscan data in an unbiased way. It begins
by performing the Fourier transform of the power spectrum
to obtain the amplitudes and phases of the standing wave components
during each time step
.
These harmonics can be written as complex coefficients
,
where n labels the harmonic by
the number of full periods of the wave across the
spectral band and
indicates that the coefficients are expected to
change with time, as the spectra are recorded in discrete time steps.
In principle, the Fourier analysis of a string of real numbers, such as
these spectra, produces one half as many complex harmonic coefficients
as there were spectral channels in the
power spectrum, but, in practice, the standing waves
arise from significant signal only at low values of n.
Thus, the standing wave content of an image-formatted database can
be described by another ``image'' (or table)
of complex numbers, with the same number
of time steps, but many fewer values for
than are
required for the number of channels in the spectrum
.
Figure 4 shows the time behavior of the harmonic content of the
first 63 harmonics in the Arecibo data image in the left part of the figure.
The standing waves appear with a variety of periodicities, with
several long-lived bursts in the harmonics around n=20, which corresponds to
differential delays
sec, the round-trip light travel
time between the Arecibo feed support structure
and the surface of the reflector.
There is substantial variability depending on where the scatterer is
located on the support structure.
There are also some bursts of signal in the lowest
harmonics, possibly due to differential delays
between scattered paths such as R3 and R2 in
Figure 3, which are both scattered downward into the dish from different
points on the support structure; alternatively, there could be scattering
from point S2 directly in the direction of the feed F, which would
also cause a fairly short differential
delay and thus a long period standing wave.
The harmonic signature of a bright galaxy can also
be seen near the midpoint of the data set. The faint, periodic, horizontal
striping is a result of the slightly variable correlator dump time, causing the
record integration time to beat with the 7 second grid spacing to
which the data was interpolated.
Phase drift of an n harmonic standing wave is described by watching the phase
term
from
vary with time.
Figure 5 shows an example of the amplitude and phase data for a single
harmonic n=15. The time variation of both
and
can be efficiently tracked in time by
sliding a window of 16 to 128 time steps along the table of
and then taking the Fourier transform of the complex time series
of each harmonic within the windowed region.
A recipe for tracking and modeling a standing wave is summarized as follows:
(1) Compute the table (or image) of complex harmonic coefficients
(2) Separate the complex coefficients of the nth harmonic as a function of time into a single long vector (such as the data plotted in Figure 5).
(3) Subdivide the vector into short enough time
spans that the rate of drift is nearly constant over that time window.
The choice of length for the time window depends on
how rapidly the rate of drift changes, since the window must be short enough
to track changes in the drift rate but also long enough to be immune to
signals that are localized in a single beam. Of course, a choice
for the window length of
time steps (with N equal to an
integer in the range 4 to 7)
helps to increase the efficiency in computing the transform.
(4)
The phase interpolation needed to track the waves is simplified if there
is overlap of the windows, and therefore the window was advanced
by either
or
time steps before
recomputing the transform.
Thus, a mathematical summary is: each window contains
points taken from
with
running
from
to
. The Fourier transform of this series of p
numbers produces p complex coefficients
.
Here
is the strength of the component drifting at
rate
with phase
at time
.
In principle,
there may be well be a range of different standing wave drift rates
contributing at any given time,
since many locations on the support structure are capable of scattering.
In practice, for each window, we tabulated a
and a
corresponding to the
and
of the
strongest
component in each time window, after
checking for significance relative to the noise level.
(5) Depending of the degree of overlap of the windows, each time
step
falls in either 2 or 4 windows. Each window that produced
valid measurements for
and
can be used to
form an estimate of the standing wave phase at
. Thus,
a reasonable method for tracking the phase for the nth harmonic is
to compute an estimate
for the phase at each time
from the weighted vector average of the overlapping windows:
![]()
The sums are taken over the 2 (or 4) windows
that overlap at
. The weighting factors
include
, which indicates the statistical significance of
the solution for the window w, and a factor
,
which gradually
transfers the weight among the windows by assigning the greatest emphasis to
the solution whose window is centered closest to
. The factor
is
one of many possible weight adjustments. An amplitude
also results
from the vector average;
is close to unity when there is close
agreement between the phase determined by all the windows included in the
average.

Figure 5: Amplitude and phase for the n=15 harmonic standing wave.
Top panel. Coefficient amplitudes plotted as a function of time
step (light noisy curve).
The heavy solid points are vector averages of the amplitude (for
20 time steps), computed after application of the phase tracking
algorithm. Heavy points are plotted only when the amplitude surpasses
a set threshold.
Bottom panel. Standing wave phases (points). Smooth interpolated
curve results from the phase tracking algorithm. The curve is lighter
in regions where the signal to noise ratio for the wave is low.
(6) Once a solution for phase tracking has been performed
(such as shown in the lower panel of Figure 5), a model
for the temporal behavior of the wave amplitudes
can be made by smoothing the time sequence of
. When the resulting wave
amplitudes surpass a set
threshold for significance, they can be stored in a table of
harmonic coefficients that can subsequently be used to generate models
for the standing waves
as a function of time (as shown in Figure 6) and then correct
the observations
by subtracting the standing wave model from the data image.
Note that this technique succeeds at doing little damage to the celestial
signals, since galaxies typically fall in only one beam and the fits are
derived from many beams. This approach is far superior to simply ``nulling''
the
component, since this would throw away genuine information from the sky that is specific to each beam.

Figure 6: Standing wave edits.
Left panels. Versions of the data image in Figure 4, but with
standing wave models subtracted. The data images are presented on the
same grayscale wedge as Figure 4.
Right panels. Standing wave models built from harmonic analysis
of the data image in Figure 4, followed by application of a phase
tracking algorithm and reconstruction of a noise-free images of the standing waves. The upper model includes harmonics n= 4 through 25, when they
are deemed significant. The lower model includes n= 1 through 25. The
grayscale is about
more sensitive for the models than for the
data images.
While our experience at Arecibo and Nancay has shown that the strongest standing waves are due to the sun, we have also seen similar, but weaker, standing waves at night at Arecibo when observing in the vicinity of the strong radio source Taurus A (the Crab Nebula); in this case, the pattern repeated at the same sidereal time day after day. Very strong standing waves have also been generated by faulty equipment that generated intermittent, broadband noise; these waves had fixed phase in successive scans, since the source of the rfi was fixed to the Earth and the antenna was stationary during the observation.
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Next Section: Final Comments Title/Abstract Page: Driftscan Surveys in the Previous Section: The technique | Contents Page: Volume 14, Number 1 |