Extended Data Fig. 10: Simulated soil C changes to warming under three precipitation levels.
From: Drought amplifies warming-induced soil carbon loss in a decade-long experiment
(a–c) Simulated changes of surface (0-15 cm) soil C, MAOM, and POM. Model simulations were conducted under two conditions: with and without considering the changes of microbial parameters. The error bar represents mean ± S.E.M. (n = 11 yearly simulations). (d, e) Simulated soil C changes in MAOM and POM under multiple warming scenarios, where varying temperature increases were imposed on ambient temperatures across three precipitation levels. Plant, microbial parameters, and moisture were held constant across warming treatments to isolate the temperature effect only. The error bar represents mean ± S.E.M. (n = 11 yearly simulations).
