Next: 10.3.5 The program FLUX
Up: 10.3 Flux Calibration (visitor's
Previous: 10.3.3 Determining the absolute
Subsections
In the final amplitude calibration performed on the source (see next section), the
flux of the source is determined by reference to the flux of the amplitude
calibrator which is usually also the phase calibrator. This means that the averaged
efficiencies
computed by SOLVE FLUX and the automatic procedure are
not directly used and in many case variations of
does not affect the
accuracy of the final amplitude calibration because they are corrected. It is then
fundamental to have a good estimate of the flux of the amplitude calibrator but not
necessarily to know precisely the averaged
.
Using the automatic procedure, the possible biases are the following:
- 1.
- There is some shadowing on the reference source, the estimate
of the
can be wrong. Use another reference.
- 2.
- One or several antennas are off focus:
is larger than
but flux densities can still be correct if there is no significant drift during the
time interval used to measure the fluxes. If the data are affected by a significant
focus drift, it also affects the accuracy of the flux measurements. Depending of the
observation time of the reference and of the sources, the estimated flux densities
can be either too low (reference taken at the beginning when the focus is correct,
sources at the end when the focus is off) or too high (opposite situation). In both
cases, it is necessary to check the focus (data called FOCUS or have a look to
the show.ps file). In the first case, the measured fluxes are correct. In the
second case, the flux calibration must be done on a smaller interval of time where
the focus drifts remain negligible.
- 3.
- The pointing on the reference is bad,
is overestimated implying
that the flux of all other sources (with good pointing) is also overestimated.
Check the pointing on the possible reference sources (data called POINT
or have a look to the show.ps file) and select a better reference.
- 4.
- There is a strong atmospheric decorrelation. Flux measurements
are performed on cross-correlations of about 4 minutes and the atmospheric phase
fluctuations are high (check them on an individual cross-correlation taken on a
strong quasar e.g. the RF calibrator), there are two possibilities: i) the
atmospheric correction works well (clear sky), this is usually the case and it is
necessary to apply it to measure the fluxes or 2) the atmospheric correction does
not work (cloudy sky), the data can be used at 3mm and the flux scale can be
computed by selecting the best scans on a small interval of time but at 1.3mm data
are useless.
- 5.
- The interferometric efficiencies
are really very different
to
because there is a wonderful mixing of the points mentioned above... Ask
to an expert (your local contact first, myself later if needed...).
Note that the biases 3) and 4) do not affect flux estimates when they are performed
on pointing data (like in the case of the flux sessions).
Next: 10.3.5 The program FLUX
Up: 10.3 Flux Calibration (visitor's
Previous: 10.3.3 Determining the absolute
S.Guilloteau
2000-01-19