Table 2
Summary of results from the four LOFAR pulsar observing campaigns and WSRT observation.
PSR | Date | Telescope | Station(s) | FWHM RMSF | σ inst |
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RM![]() |
[dd.mm.yy] | [rad m-2] | [rad m-2] | [rad m-2] | CODE | [rad m-2] | ROB | [rad m-2] | |||
|
||||||||||
B0834+06 | 11.04.11 | LOFAR | Superterp | 6.2 | 0.20 | 25.15 ±0.18 | 0.52 | N/A | N/A | 23.6 ± 0.7 |
B0834+06 | 20.10.11 | LOFAR | Superterp | 9.4 | 0.20 | 24.94 ± 0.24 | 0.64 | N/A | N/A | 23.6 ± 0.7 |
B1642−03 | 23.03.12 | LOFAR | Superterp | 6.6 | 0.20 | 15.98 ± 0.23 | 0.8 | 16.04 ± 0.18 | 1.3 | 15.8 ± 0.3 |
B1919+21 | 23.03.12 | LOFAR | Superterp | 0.8 | 0.08 | –16.95 ± 0.12 | 0.5 | –16.92 ± 0.07 | 1.3 | –16.5 ± 0.5 |
B2217+47 | 23.03.12 | LOFAR | Superterp | 6.6 | 0.13 | –35.72 ± 0.15 | 1.0 | –35.60 ± 0.11 | 1.1 | –35.3 ± 1.8 |
B0834+06 | 22.04.12 | WSRT | N/A | 12.0 | 1.2 | 25.4 ± 1.8 | N/A | 25.1 ± 1.5 | N/A | 23.6 ± 0.7 |
B0834+06 | 10.07.12 | LOFAR | Superterp | 4.2 | 0.07 | 25.16 ± 0.13 | 0.5 | 25.23 ± 0.08 | 0.9 | 23.6 ± 0.7 |
B0834+06 | 10.07.12 | LOFAR | FR606 | 4.2 | 0.10 | 25.21 ± 0.15 | 0.4 | 25.16 ± 0.10 | 1.2 | 23.6 ± 0.7 |
B0834+06 | 10.07.12 | LOFAR | SE607 | 4.2 | 0.15 | 25.22 ± 0.18 | 0.6 | 25.39 ± 0.14 | 1.0 | 23.6 ± 0.7 |
Notes. Columns 1–11 show the pulsar observed, date (see Table 1 for specific times), the telescope, the LOFAR
stations (if applicable, see Table 1 for
specific station names), the FWHM of the RMSF from RM-synthesis, the error
introduced by instrumental effects σinst, the Faraday
depth of the ISM toward the pulsar φISM as determined
using the CODE TEC maps, the reduced chi-squared value
for
comparison between the ionospheric Faraday depths from ionFR
using CODE TEC data and the observed Faraday depths, the Faraday depth
of the ISM toward the pulsar φISM as determined using
the ROB TEC maps, the reduced chi-squared value for comparison between the
ionospheric Faraday depth produced from ionFR using CODE TEC
data and the observed Faraday depths. The final column gives the catalog RM value
from psrcat (Manchester et al. 2005) for
comparison. Note that ROB TEC maps were not available for the observations of
B0834+06 taken in 2011. Since a single observation was obtained with WSRT, the
reduced chi-squared value is not applicable because the Faraday depth of the ISM was
determined by subtracting the Faraday depth of the ionosphere from the observed
Faraday depth.
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