Table 3.
Maximum anisotropy direction for every scaling relation, together with the needed H0 relative variation to fully explain the anisotropy.
| Scaling | Max. anisot. | H0 | Bootstrap | MC |
|---|---|---|---|---|
| relation | direction (l, b) | variation (%) | significance (σ) | p-value (σ) |
| Our sample | ||||
| LX − T | (274° , −9° ) |
8.7 ± 3.1% | 2.8σ | p = 0.016 (2.4σ) |
| YSZ − T | (268° , −16° ) |
14.0 ± 3.4% | 4.1σ | p = 0.011 (2.6σ) |
| LBCG − T | (257° , −12° ) |
9.1 ± 4.8% | 1.9σ | p = 0.420 (0.8σ) |
| Our sample+ACC | ||||
| LX − T | (284° , −4° ) |
9.3 ± 3.1% | 3.0σ | p = 8.8 × 10−4 (3.3σ) |
| YSZ − T | (276° , −14° ) |
13.3 ± 3.1% | 4.3σ | p = 1.9 × 10−4 (3.8σ) |
| All combined | (273° , −11° ) |
9.0 ± 1.7% | 5.4σ | p = 3.4 × 10−9 (5.9σ) |
Notes. The statistical significances derived by the default bootstrap method and by the MC isotropic simulations are also listed. The MC p-values account for both the amplitude of the anisotropies, and the agreement in their directions. The Gaussian σ values that correspond to the p-values are also listed, for easier comparison.
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