Rapid Phase Calibration and the Atmospheric Phase Interferometer (API)
For some objects, and under suitable weather conditions, the phase calibration can be considerably improved by rapidly switching between the source and calibrator. Source-Calibrator observing cycles as short as 40 seconds can be used for very small source-calibrator separations. However, observing efficiency declines for very short cycle times, so it is important to balance this loss against a realistic estimate of the possible gain. Experience has shown that cycle times of 100 to 150 seconds at high frequencies have been effective for source-calibrator separations of less than 10 degrees. For the old VLA this was known as "fast-switching." For the upgraded VLA it is just a loop of source-calibrator scans with short scan length. This technique "stops" tropospheric phase variations at an "effective" baseline length of ∼vat/2 where va is the atmospheric wind velocity aloft (typically 10 to 15 m/sec), and t is the total switching time. It has been demonstrated to result in images of faint sources with diffraction-limited spatial resolution on the longest VLA baselines. Under average weather conditions, and using a 120 second cycle time, the residual phase at 43 GHz should be reduced to ≤ 30 degrees. Note, however, that for the compact D-configuration, and a typical wind velocity, this "effective" baseline length is the same as, or larger than, the longest baseline in the array, and it is not worth the increased overhead of short cycle times. Under these circumstances it is sufficient to calibrate every 5-10 minutes to track the instrumental changes. The fast switching technique will also not work in bad weather (such as rain showers, or when there are well-developed convection cells - most notably, thunderstorms). It is also important to specify correctly the required tropospheric phase stability as measured by the Atmospheric Phase Interferometer at observe time (see below).
Further details can be found in VLA Scientific Memos # 169 and 173. These memos, and other useful information, can be obtained from References 9 and 10 in Documentation. See also the High Frequency Observing guide for additional recommendations on observing at high frequencies.
An Atmospheric Phase Interferometer (API) is used to continuously measure the tropospheric contribution to the interferometric phase using an interferometer comprising two 1.5 meter antennas separated by 300 meters, observing an 11.7 GHz beacon from a geostationary satellite. The API data are heavily used for the dynamic scheduling of the VLA.
Characteristic seasonal averages are represented in Table 9 below:
| Month | API (night) [deg] | API (median) [deg] | API (day) [deg] | Wind (night) [m/s] | Wind (median) [m/s] | Wind (day) [m/s] |
|---|---|---|---|---|---|---|
| January | 2.3 | 2.8 | 3.6 | 1.6 | 1.9 | 2.3 |
| February | 2.9 | 3.4 | 4.5 | 4.0 | 4.3 | 4.5 |
| March | 2.8 | 3.7 | 5.5 | 3.4 | 3.9 | 4.7 |
| April | 3.3 | 4.5 | 6.2 | 5.3 | 5.5 | 5.8 |
| May | 2.9 | 4.6 | 6.7 | 2.6 | 3.2 | 3.7 |
| June | 3.8 | 5.5 | 7.4 | 2.5 | 3.9 | 6.3 |
| July | 6.2 | 8.3 | 10.5 | 2.9 | 2.9 | 3.0 |
| August | 5.4 | 7.1 | 11.3 | 1.7 | 2.3 | 3.0 |
| September | 5.2 | 6.6 | 8.8 | 2.3 | 3.0 | 3.6 |
| October | 4.2 | 5.3 | 7.4 | 2.3 | 2.9 | 3.7 |
| November | 2.6 | 3.0 | 4.0 | 1.2 | 2.5 | 1.6 |
| December | 2.8 | 3.2 | 4.1 | 1.2 | 1.6 | 2.7 |
- Note: day indicates sunrise to sunset values; night indicates sunset to sunrise values.
