Extended Data Fig. 10: Tropical temperature in CTL versus experiment A.
From: Soil moisture–atmosphere feedback dominates land carbon uptake variability
a, IAV in tropical (24° N to 24° S) mean land temperature in model experiments with and without variability in soil moisture (similar to Fig. 1a for NBP). b, Apparent sensitivity of global mean NBP to tropical mean temperature in CTL and experiment A.
