Skip to main content
. 2024 Aug 2;15:6555. doi: 10.1038/s41467-024-50886-w

Fig. 3. Area-weighted average of site-level climate excursion frequency through the Holocene.

Fig. 3

At each site, parametric uncertainty is considered, and the fraction of detected excursions for both directions in (a) temperature, and (b) hydroclimate range from 0 to 1. The occurrence and significance of (c) combined warm/wet and cold/dry excursions is shown as the product of wet/warm and cold/dry excursion frequency. Each bar shows the area- and uncertainty-weighted proportion of records with excursions in 400 ± 100 year windows. The axes for cold, dry, and cold/dry excursions are inverted. The excursion detection analysis is repeated in 200-year intervals across the Holocene. Colored lines show the 95% confidence interval (cl) based on null hypothesis testing. Due to test multiplicity however, we expect some apparently significant results to occur due to chance alone. Cross-hatched and single-hatched bars indicate intervals that remain significant at the 0.05 and 0.10 levels, respectively, after using a modified Holm–Bonferroni correction. See text for details.