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Table A.1.
Best solutions for α = 20 d.
| Paper II | This paper | |
|---|---|---|
| ΔtAB (d) | 47 | 48 |
| ΔmAB(2009) | 0.349 | 0.348 |
| ΔmAB(2012) | 0.419 | 0.417 |
| ΔmAB(2013) | 0.133 | 0.139 |
| ΔmAB(2014) | 0.118 | 0.116 |
| ΔmAB(2015) | 0.304 | 0.302 |
| ΔmAB(2016) | – | 0.189 |
| ΔmAB(2017) | – | 0.159 |
| ΔmAB(2018) | – | 0.261 |
| ΔmAB(2019) | – | 0.136 |
Notes. The time-dependent magnitude offset ΔmAB(t) = mA(t)−mB(t + ΔtAB) is assumed to be constant within each season. All seasonal offsets are positive because we use the opposite sign to that in Paper II.
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