General Guidelines for Phase Calibration

Adequate phase calibration is a complicated function of source-calibrator separation, frequency, array scale, and weather. And, since what defines adequate for some experiments is completely inadequate for others, it is impossible to define any simple guidelines to ensure adequate phase calibration in general. However, some general statements remain valid most of the time. These are given below.

• Tropospheric effects dominate at wavelengths shorter than 20 cm, ionospheric effects dominate at wavelengths longer than 20 cm.
• Atmospheric (troposphere and ionosphere) effects are nearly always unimportant in the C and D configurations at L and P bands, and in the D configuration at X and C bands. Hence, for these cases, calibration need only be done to track instrumental changes - once per hour is generally sufficient.
• If your target object has sufficient flux density to permit self-calibration, there is no need to calibrate more than once hourly.
• The smaller the source-calibrator angular separation, the better. In deciding between a nearby `S' calibrator, and a more distant `P' calibrator, the nearby calibrator is usually the better choice.
• At high frequencies, and longer configurations, rapid switching between the source and nearby calibrator is often helpful. See the following section.