Table 3
Transverse RM gradients.
| Source | Ref. | Implied current† | Comments |
|---|---|---|---|
| Firm, ≥2.8σ or confirmed | |||
| 0059 + 581 | * | Out | Reversal |
| 0133 + 476 | * | Out | |
| 0212 + 735 | G17* | In | Reversal |
| 0256 + 075 | G15b | In | |
| 0300 + 470 | G17 | In | |
| 0305 + 039 | G17 | In | |
| 0333 + 321 | G14 | In | |
| 0355 + 508 | G15b | Out | |
| 0403 − 132 | * | In | Possible reversal |
| 0415 + 379 | G17 | In | |
| 0430 + 052 | Go11 | In | |
| 0446 + 112 | * | Out | |
| 0552 + 398 | * | In | |
| 0716 + 714 | M13 | In | Reversal |
| 0735 + 178 | G15b | In | |
| 0738 + 313 | G14 | Out | |
| 0745 + 241 | G15b | In | |
| 0748 + 126 | G15b | In | |
| 0820 + 225 | G15b | In | |
| 0823 + 033 | G15b | Out | |
| 0834 − 201 | * | Out | |
| 0859 − 140 | * | In | Reversal |
| 0923 + 392 | G14 | In | Reversal |
| 0945 + 408 | G17 | In | |
| 0955 + 476 | * | In | |
| 1124 − 186 | * | In | |
| 1156 + 295 | G15b | In | |
| 1218 + 285 | G15b | In | |
| 1226 + 023 | H12 | Out | |
| 1334 − 127 | G15b | Out | |
| 1502 + 106 | G17 | Out | |
| 1504 − 166 | * | In | |
| 1611 + 343 | G17* | Out | |
| 1633 + 382 | G14 | In | |
| 1641 + 399 | *MG17 | In | |
| 1652 + 398 | G15b | Out | |
| 1749 + 096 | G15b | In | |
| 1749 + 701 | M13 | In | Reversal |
| 1807 + 698 | G15b | In | |
| 1908 − 201 | * | In | |
| 2007 + 777 | G15b | Out | |
| 2037 + 511 | G14 | In | Reversal |
| 2155 − 152 | G15b | In | |
| 2216 − 038 | * | In | |
| 2230 + 114 | H12 | In | |
| 2345 − 167 | G14 | Out | |
| 2351 + 456 | * | In | |
| Significant RM gradients showing time variability | |||
| 0836 + 710 | G14, MG17 | ||
| 1150 + 812 | G14* | Possible reversal | |
| 1803 + 784 | M09 | ||
| 2005 + 403 | G17* | ||
| 2200 + 420 | G17, MG17 | ||
Notes. G14 = Gabuzda et al. (2014); G15b = Gabuzda et al. (2015b); G17 = Gabuzda et al. (2017); Go11 = Gómez et al. (2011); H12 = Hovatta et al. (2012); M09 = Mahmud et al. (2009); Mahmud et al. (2013); MG17 = Motter & Gabuzda (2017). ( *) this paper; (†) current corresponding to direction of innermost gradient is given for sources displaying reversals.
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