Extended Data Fig. 4: Sensitivity of global and regional proxy-model agreement to different proxy types.
From: Tropical response to ocean circulation slowdown raises future drought risk
Global (a) and regional (b–f) agreement between hydroclimate changes reconstructed using different combinations of two proxy types and the simulated responses associated with cooling patterns in the North Atlantic. Dotted, solid, and dashed lines correspond to ensemble-mean responses from simulations with stronger, moderate, and muted cooling over the tropical North Atlantic respectively. Model-proxy agreement is quantified using the Cohen’s κ metric.
