Robustness
Which conclusions survive a change of mind?
Temporal aggregation, baseline period, variable and dataset, which orbital terms are allowed, detrending, spectral resolution, resampling, smoothing and chronology error. Some results do not move at all; others move a lot, and the paper is scoped to match.
Smoothing manufactures orbital peaks, unless the null knows about it
Pure AR(1) noise, φ = 0.942 (matched to LR04 at 2 ka), n = 401, 100 replicates
100-kyr band
- naive null
- smoothing-aware null
41-kyr band
- naive null
- smoothing-aware null
A counterfactual orbit can fit better than the real one
R² of the admissible one-pole model, Berkeley Earth
- real forcing
- circular orbit (obliquity only)
- eccentricity only (no tilt)
Coarser aggregation inflates everything
Eccentricity detectability ratio by temporal resolution (NCEP)
- monthly (9 residual dof)
- bimonthly (3)
- seasonal (1)
Precession coherence needs an accurate clock
Median coherence at 23 kyr under random age-model error (40 draws each)
- LR04
- EPICA Dome C
- Cheng 2016
Which orbital predictor carries each record?
Cross-validated R² of a one-pole linear response; filled = beats 300 phase-randomised surrogates (p < 0.05)
- LR04
- EPICA Dome C
- Cheng 2016
Explore every row
2,939 statistics across 14 axes. Pick an axis and a statistic; rows are regions (A) or records (B), columns are settings.
| Region | 1951-1980 | 1981-2010 | 1991-2020 | 1948-2024 |
|---|---|---|---|---|
| NH extratropics | land | 0.998 | 0.997 | 0.997 | 0.998 |
| NH extratropics | ocean | 0.992 | 0.991 | 0.989 | 0.991 |
| SH extratropics | land | 0.996 | 0.994 | 0.994 | 0.996 |
| SH extratropics | ocean | 0.998 | 1.000 | 1.000 | 1.000 |
| Tropics | land | 0.315 | 0.183 | 0.196 | 0.248 |
| Arctic | all | 0.992 | 0.989 | 0.985 | 0.989 |
| Sahel | 0.934 | 0.973 | 0.970 | 0.958 |
| Southern Ocean | 0.998 | 0.999 | 0.999 | 0.999 |
| Global | all | 0.000 | 0.000 | 0.000 | 0.000 |