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Fig. 5 Density plots showing the relationship between growth responses to extreme events and site-level mean precipitation from all sites (N = 1314). Density plots showing the relationship between growth responses to extreme events and site-level mean precipitation from all sites (N = 1314). (A and B) Relationship between log-transformed cool-season mean precipitation and, respectively, the proportion of years with extremely low and high cool-season precipitation that are also years with extremely low and high growth, after correcting for chance agreement using Cohen’s κ. (C and D) Relationship between log-transformed warm-season mean precipitation and, respectively, the proportion of years with extremely low and high warm-season precipitation that are also years with extremely low and high growth, after correcting for chance agreement using Cohen’s κ. The linear relationship between log-transformed mean precipitation and growth responses to extremes is shown with blue lines (cool season) and red lines (warm season) for those with significant (P < 0.05) relationships, along with Spearman’s rank correlation coefficient (ρ). Matthew P. Dannenberg et al. Sci Adv 2019;5:eaaw0667 Copyright © 2019 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).
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