2021A&A...647A..84T


Query : 2021A&A...647A..84T

2021A&A...647A..84T - Astronomy and Astrophysics, volume 647A84-84 (2021/3-1)

The impact of solar wind variability on pulsar timing.

TIBURZI C., SHAIFULLAH G.M., BASSA C.G., ZUCCA P., VERBIEST J.P.W., PORAYKO N.K., VAN DER WATEREN E., FALLOWS R.A., MAIN R.A., JANSSEN G.H., ANDERSON J.M., BAK NIELSEN A.-S., DONNER J.Y., KEANE E.F., KUNSEMOLLER J., OSLOWSKI S., GRIESSMEIER J.-M., SERYLAK M., BRUGGEN M., CIARDI B., DETTMAR R.-J., HOEFT M., KRAMER M., MANN G. and VOCKS C.

Abstract (from CDS):


Context. High-precision pulsar timing requires accurate corrections for dispersive delays of radio waves, parametrized by the dispersion measure (DM), particularly if these delays are variable in time. In a previous paper, we studied the solar wind (SW) models used in pulsar timing to mitigate the excess of DM that is annually induced by the SW and found these to be insufficient for high-precision pulsar timing. Here we analyze additional pulsar datasets to further investigate which aspects of the SW models currently used in pulsar timing can be readily improved, and at what levels of timing precision SW mitigation is possible.
Aims. Our goals are to verify: (a) whether the data are better described by a spherical model of the SW with a time-variable amplitude, rather than a time-invariant one as suggested in literature, and (b) whether a temporal trend of such a model's amplitudes can be detected.
Methods. We use the pulsar timing technique on low-frequency pulsar observations to estimate the DM and quantify how this value changes as the Earth moves around the Sun. Specifically, we monitor the DM in weekly to monthly observations of 14 pulsars taken with parts of the LOw-Frequency ARray (LOFAR) across time spans of up to 6 years. We develop an informed algorithm to separate the interstellar variations in the DM from those caused by the SW and demonstrate the functionality of this algorithm with extensive simulations. Assuming a spherically symmetric model for the SW density, we derive the amplitude of this model for each year of observations.
Results. We show that a spherical model with a time-variable amplitude models the observations better than a spherical model with a constant amplitude, but that both approaches leave significant SW-induced delays uncorrected in a number of pulsars in the sample. The amplitude of the spherical model is found to be variable in time, as opposed to what has been previously suggested.

Abstract Copyright: © ESO 2021

Journal keyword(s): pulsars: general - solar wind - ISM: general - gravitational waves

Simbad objects: 50

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Number of rows : 50
N Identifier Otype ICRS (J2000)
RA
ICRS (J2000)
DEC
Mag U Mag B Mag V Mag R Mag I Sp type #ref
1850 - 2026
#notes
1 PSR J0030+0451 Psr 00 30 27.42348 +04 51 39.7144           ~ 596 1
2 PSR B0031-07 Psr 00 34 08.9100 -07 21 56.000           ~ 350 0
3 PSR J0034-05 Psr 00 34 21.8281 -05 34 36.620           ~ 201 0
4 PSR J0051+0423 Psr 00 51 30.1 +04 22 49           ~ 24 0
5 PSR J0137+1654 Psr 01 37 23.88 +16 54 42.1           ~ 17 0
6 PSR B0148-06 Psr 01 51 22.71800 -06 35 02.9800           ~ 112 0
7 PSR J0218+42 Psr 02 18 06.3604 +42 32 17.365           ~ 365 2
8 PSR B0301+19 Psr 03 04 33.115 +19 32 51.40           ~ 247 0
9 PSR J0407+16 Psr 04 07 54.939 +16 07 16.40           ~ 35 1
10 PSR B0523+11 Psr 05 25 56.49800 +11 15 18.8000           ~ 125 1
11 PSR B0525+21 Psr 05 28 52.308 +22 00 01.00     14.30     ~ 370 0
12 V* CM Tau Psr 05 34 31.9474694616 +22 00 52.153698024           ~ 5476 0
13 PSR J0538+2813 Psr 05 38 25.06 +28 17 11.0           ~ 224 1
14 PSR J0540+3207 Psr 05 40 37 +32 07.6           ~ 18 0
15 PSR B0540+23 Psr 05 43 09.65 +23 29 06.1     14.40     ~ 278 0
16 PSR J0609+2130 Psr 06 09 58.8861 +21 30 02.840           ~ 22 0
17 PSR B0609+37 Psr 06 12 44.087 +37 21 40.20           ~ 62 0
18 PSR B0611+22 Psr 06 14 17.0324288405 +22 29 57.017874999           ~ 285 0
19 PSR B0626+24 Psr 06 29 05.7273 +24 15 41.546           ~ 123 0
20 PSR B0656+14 Psr 06 59 48.18800 +14 14 19.2000   24.85 24.90     ~ 943 1
21 PSR J0740+6620 Psr 07 40 45.799 +66 20 33.60           ~ 395 0
22 PSR J0823+0159 Psr 08 23 09.78731 +01 59 12.6003           DA 244 0
23 PSR B0823+26 Psr 08 26 51.5068 +26 37 21.297           ~ 541 1
24 PSR B0834+06 Psr 08 37 05.64620 +06 10 15.8700           ~ 472 0
25 PSR B0940+16 Psr 09 43 30.10 +16 31 37.0           ~ 79 0
26 PSR B0950+08 Psr 09 53 09.31210 +07 55 36.9000           ~ 806 2
27 PSR J1022+10 Psr 10 22 57.990 +10 01 52.92           ~ 279 2
28 PSR J1025-07 Psr 10 24 38.6991893112 -07 19 19.045523388     19.81 18.78 18.00 ~ 286 1
29 PSR J1125+7819 Psr 11 25 59.851 +78 19 48.70           ~ 36 0
30 PSR B1133+16 Psr 11 36 03.09460 +15 51 15.9000           ~ 715 0
31 PSR B1257+12 Psr 13 00 03.1075 +12 40 55.155           ~ 546 1
32 PSR J1400-1431 Psr 14 00 37.00370 -14 31 47.0422           ~ 49 0
33 PSR B1540-06 Psr 15 43 30.1373 -06 20 45.332           ~ 131 1
34 PSR B1604-00 Psr 16 07 12.078 -00 32 40.98           ~ 228 1
35 PSR J1640+2224 Psr 16 40 16.744850 +22 24 08.84119           ~ 210 0
36 PSR B1642-03 Psr 16 45 02.0330 -03 17 57.200           ~ 394 0
37 PSR B1702-19 Psr 17 05 36.09300 -19 06 39.2000           ~ 191 1
38 PSR J1730-2304 Psr 17 30 21.68471 -23 04 31.2590           ~ 194 1
39 PSR J1744-1134 Psr 17 44 29.4220844 -11 34 54.801320           ~ 323 1
40 PSR B1818-04 Psr 18 20 52.5920 -04 27 37.120           ~ 230 0
41 PSR B1822-09 Psr 18 25 30.62000 -09 35 22.0000           ~ 382 0
42 PSR B1831-04 Psr 18 34 25.62100 -04 26 15.7000           ~ 103 0
43 PSR B1845-19 Psr 18 48 18.03 -19 52 31.0           ~ 74 0
44 PSR B1857-26 Psr 19 00 47.54200 -26 00 44.8000           ~ 195 1
45 PSR B1911-04 Psr 19 13 54.16240 -04 40 47.5600           ~ 192 0
46 V* LY Aqr Psr 20 51 07.52058 -08 27 37.6100           ~ 236 2
47 PSR B2145-07.8 Psr 21 45 50.45590 -07 50 18.5900           ~ 336 0
48 PSR J2222-0137 Psr 22 22 06.00015 -01 37 15.7827           ~ 78 0
49 PSR J2256-1024 Psr 22 56 56.390 -10 24 34.37           ~ 88 0
50 PSR J2317+1439 Psr 23 17 09.235606 +14 39 31.29559           ~ 211 1

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