Up: Phase calibration scheme for
The present scheme is described with reference to the array configuration
of the GRH which has
16 antenna groups along a E-W arm and another 16 along a
South arm.
The redundant shortest baseline in the E-W arm is used along with
those formed by the multiplications
between the antenna groups in the E-W and South arm.
Consider the multiplications between the groups G1, G2,
G3 . . . G16 in the E-W arm
and G17 in the South arm. The possible closure equations are,
|  |
(1) |
|  |
(2) |
.
.
.
|  |
(15) |
These 15 equations can be solved for the
16 unknowns using
the standard singular value decomposition technique
[9, (Press et al. 1992).] The method gives the best possible solution
in the least squares sense.
It can be shown that the error due to the number of equations
being one less than the number of unknowns
is only 6% [11, (Ramesh 1999).]
The above process is repeated 16 times corresponding to
each one of the 16 groups in the South arm. In each step, a
set of 16 phases are
determined and thus at the end of
step, we have all the 256 true visibility phases that correspond to the
E-W
S multiplications. It is to be noted that in the above set of
equations, the visibility phases (
)corresponding to the redundant shortest baseline in the E-W arm is
assumed to be zero, since the baseline length is small to resolve
a source like Sun in our frequency range (40-150 MHz) of observation.
Figure 1 shows the radio map of the solar corona at 75 MHz obtained with the
GRH on April 20, 1997 using
the above method. The map made using the external calibration
method i.e., by correcting for the instrumental errors using
the observations of radio source Virgo A (which is a point
source for the GRH and happens to be close to the Sun's declination
during the month of April) is shown in Fig. 2. The similarity
between the two maps is good.
![\begin{figure}
\includegraphics [width=8cm]{exp4.eps}\end{figure}](/articles/aas/full/1999/16/ds8430/Timg10.gif) |
Figure 2:
Radio map of the Sun obtained on the same day as in Fig. 1 but using the
external calibration method
with the radio source Virgo A as the calibrator |
![\begin{figure}
\includegraphics [width=8cm]{exp2.eps}\end{figure}](/articles/aas/full/1999/16/ds8430/Timg13.gif) |
Figure 3:
Radio map of the Sun at 75 MHz made using
self-calibration technique in AIPS with the
map in Fig. 1 as the starting model. The peak brightness
in the map is K and the rms noise
is K |
A map obtained using the self-calibration technique with the map
in Fig. 1
as the starting model, is shown in Fig. 3.
One can notice that the features in the self-calibrated map are seen
more clearly
with improvement in the signal to noise ratio.
We also found that our method is quite successful in extracting
weak and diffuse features particularly during times when Sun is active
and is dominated by emission from strong and localised radio emitting
discrete source(s). Figure 4 shows one such map obtained on
September 28, 1997. Although the map is dominated
by the strong source close to the limb in the S-W quadrant,
the presence of weak, diffuse features close to the
east limb can be seen clearly.
A comparison of the GRH maps shown
above with those obtained with the Nancay radioheliograph at 164 MHz
indicates that our method works reasonably well.
![\begin{figure}
\includegraphics [width=8cm]{exp3.eps}\end{figure}](/articles/aas/full/1999/16/ds8430/Timg16.gif) |
Figure 4:
Radio map of the Sun at 109 MHz obtained using our
method. The brightness temperature of the bright source close to
the limb in the S-W
quadrant is K and that of the source close to the
east limb is K |
Up: Phase calibration scheme for
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