Source A B C
3C286 1.480 0.292 -0.124
3C48 2.345 0.071 -0.138
3C147 1.766 0.447 -0.184
NOTE: Note that the AIPS program SETJY with OPTYP = 'CALC' will calculate and insert the relevant flux densities into the database. Do not use this option if you are switching frequencies within the observing run. In this case you must calculate and insert the appropriate values for each frequency and IF with OPTYP = ' '. Note also that the 15OCT89 and preceding versions of AIPS do not correct the calculated flux densities for errors in the Baars scale (see next section), nor account for special variations based on UV restrictions.
Below are listed the RATIOS between the true and Baars et al. value for 3C48, 3C286 and 3C147 at the various frequencies for 1987 and 1989. Multiply the Baars et al. value by this ratio to obtain the correct flux density: Time variability is small compared to the offsets. See R. Perley if you need more information.
1987 1989
P L C X U P L C X U
3C48 0.95 1.02 1.04 1.06 1.10
3C147 1.00 0.97 0.95 0.97 1.01 To be determined in Jan. 1990.
3C286 0.95 1.00 1.01 1.01 1.02
Careful observations have allowed the following set of rules to be established for accurate bootstrapping of flux densities using 3C286 or 3C48. For 3C147, use the rules for 3C48.
3C286 is partially resolved to most combinations of configuration and band. Its resolution occurs on two different scales - there is a weak secondary located 2.5" from the core, and the core itself is partially resolved on longer baselines. Nevertheless, 3C286 can be used as a flux calibrator for all VLA observations providing the rules laid down below are followed.
3C48 and 3C147 are heavily resolved to some combinations of configuration and frequency, but nevertheless can be preferable as a flux calibrator over 3C286 since they contain no extended structure on scales greater than 1". Use of 3C48 or 3C147 for flux calibration is preferred over 3C286, providing the former can be used for the array configuration and band under consideration.
3C48/3C147 90cm All configurations 20cm C and D configurations 6cm D configuration 3.6cm D configuration 3C286 90cm B,C,D configurations 20cm C and D configurations 6cm D configuration 2cm D configuration 1.3cm D configuration
NUMBER OF
SOURCE BAND UVRANGE CONFIG INNER ANTENNAS NOTES
(cm) (K) (per arm)
--------------------------------------------------------------------------
3C48/3C147 90 0-40 All All
3C48/3C147 20 0-40 A 7
" B,C,D All
3C48/3C147 6 0-40 A 3
" B,C,D All
3C48/3C147 3.6 0-40 A 2
" B 6
" C,D All
3C48/3C147 2 0-40 A 1 Not recommended
" B 4
" C,D All
3C48/3C147 1.3 0-40 A 1 Not recommended
" B 3
" C,D All
NUMBER OF
SOURCE BAND UVRANGE CONFIG INNER ANTENNAS NOTES
(cm) (K) (per arm)
-----------------------------------------------------------------------
3C286 90 0-18 A 7
" B,C,D All
3C286 20 0-18 A 4
" B,C,D All
90-180 A All Reduce flux by 6%
3C286 6 0-25 A 1 Not recommended
" B 4
" C,D All
150-300 A All Reduce flux by 2%
3C286 3.6 50-300 A 3 Reduce flux by 1%
50-300 B 7 Reduce flux by 1%
50-300 C All Reduce flux by 1%
0-15 D All
3C286 2 0-150 A 3
" B,C,D All
3C286 1.3 0-185 A 2
" B 7
" C,D All
If these guidelines are followed, the bootstrap accuracy should be 1 or
2 percent at the two lower bands, and perhaps 3 to 5 percent at the upper
bands. At 2cm and 1.3cm bands, other effects, such as dish efficiency,
pointing and atmospheric absorption (1.3cm) are probably more important.
If one were to ignore the guidelines, and blindly calibrate the data on the basis of the available data, the flux error obtained would vary according roughly to how much resolution occurs but would not exceed 5% for 3C286. Bear in mind that there will occur a differential error as well, as the antennas at the ends of the array will be overcalibrated with respect to those at the center.
1) L-band 1+(1.3x10-3)(freq-1465) (1400-1670 MHz) 2) C-band 1+(3.3x10-4)(freq-4885) (4500-4950 MHz) 3) U-band No correction needed, 14650-15300 MHzDue to uncertainties in system behavior, this scheme has not yet been implemented at P and K bands. The coefficients have not been determined at X-band.
It now seems profitable for anyone interested in the highest positional accuracy to use J2000 coordinates for all future observations, unless compatibility with previous observations is critical and the whole series does not span enough time to be unduly confused by the known error in Newcomb's precession constant. (It is probably less work to put previous observations in J2000 coordinates that to calculate the corrections to the 1950 coordinates of various dates, if the observations span more than a couple of years). For the general VLA user, the pressure to change systems is not so strong--he must consider whether it is more important that his observation remain compatible with previous observations of the object, or whether it should be compatible with future accurate astrometry, either radio or optical. We do not recommend changing to J2000 coordinates for an object which you have observed here before, and might conceivably wish to combine the old (u,v) data--there is no point in just asking for trouble. However, we encourage the use of J2000 coordinates for new observations unless there is a firm argument against doing so. It seems inevitable that J2000 coordinates are going to come into general use, and the sooner we can get through the painful transition period, the better off we all shall be.
NAME EPOCH PC RA DEC
0038-213 2000.0 C 00 38 29.9524 -21 20 04.027
0036-216 1950.0 C 00 36 00.4390 -21 36 33.100
BAND FLUX A B C D UVmin UVmax
-----------------------------------------------------
20cm L 0.78 ? ? X X 10
6cm C 0.34 S S S S 200
3.6cm X 0.22 X S S S 200
NAME EPOCH PC RA DEC
0714+146 2000.0 T 07 14 04.6352 +14 36 20.629
0711+146 1950.0 T 07 11 14.3000 +14 41 33.000
Also known as 3C175.1
BAND FLUX A B C D UVmin UVmax
-----------------------------------------------------
90cm P 6 X S S X 1 4
20cm L 1.90 X X X S 4
NAME EPOCH PC RA DEC
1733-130 2000.0 A 17 33 02.7058 -13 04 49.546
1730-130 1950.0 A 17 30 13.5352 -13 02 45.837
BAND FLUX A B C D UVmin UVmax
-----------------------------------------------------
20cm L 5.20 S X X P 40 3
6cm C 5.00 P P P P
3.6cm X 5.80 P P P P
2cm U 3.70 P P P P
NAME EPOCH PC RA DEC
1759+237 2000.0 C 17 59 00.3527 +23 43 46.974
1756+237 1950.0 C 17 56 55.9320 +23 43 55.800
BAND FLUX A B C D UVmin UVmax
-----------------------------------------------------
20cm L 0.70 S S S X 6 90
6cm C 1.00 X S S S 90
3.6cm X 0.55 S S S S
2cm U 0.00 ? ? ? ?
TABLE HEADER
Line 1: Source IAU name at epoch (2000). Use
of this name in OBSERVE fetches RA
and DEC at epoch 2000.
PC = Position Code for coordinate accuracy.
Line 2: Source IAU name at epoch (1950). Use
of this name in OBSERVE fetches RA
and DEC at epoch 1950.
Line 3: (Optional)-Other common names for the
source. Desired epoch must be
explicitly specified in OBSERVE.
(The Dec. 1989 release of OBSERVE
does not recognize this alias name).
Position codes are:
A = positional accuracy <0.002 arcseconds
B = positional accuracy 0.002 - 0.01 arcseconds
C = positional accuracy 0.01 - 0.15 arcseconds
T = positional accuracy >0.15 arcseconds
Note: Errors in declination increase in the south, except for A
and B calibrators.
TABLE FORMAT
Col 1 & 2: Band and Band code. For 1.3cm use 2cm entry.
Col 3: Flux = The approximate flux density of the source.
Use only as an indicator of the source strength.
Col 4-7: Calibrator quality in the A, B, C and D configuration
P = <3% amplitude closure errors expected
S = 3-10% closure errors expected
X = Do not use. Too much resolution or too weak
? = Not observed
Col 8 & 9: Antsol restrictions. These are suggested UVLIMITS in
K to use in CALIB to avoid data which are
contaminated by structure. A UVMIN (Col. 8) generally
means the source is confused at short spacings. A
UVMAX (Col. 9) generally means the source is resolved
at long spacings.
Particular comments on the above examples are: