Observation‐based global soil heterotrophic respiration indicates underestimated turnover and sequestration of soil carbon by terrestrial ecosystem models

Soil heterotrophic respiration (R_h) refers to the flux of CO2 released from soil to atmosphere as a result of organic matter decomposition by soil microbes and fauna. As one of the major fluxes in the global carbon cycle, the estimation of global R_h still exists large uncertainties, which further limited our current understanding of the carbon accumulation in soils. Here, we applied a Random Forest algorithm to create a global dataset of soil R_h, by linking 761 field observations with both abiotic and biotic predictors. We estimated that the global R_h was 48.8 ± 0.9 Pg C yr^-1 for 1982–2018, which was 16% less than the ensemble mean (58.6 ± 9.9 Pg C yr^-1) of 16 terrestrial ecosystem models. By integrating our observational R_h with independent soil carbon stock datasets, we obtained a global mean soil carbon turnover time of 38.3 ± 11 yr. Using observation-based turnover times as a constraint, we found that terrestrial ecosystem models simulated faster carbon turnovers, leading to a 30% (74 Pg C) underestimation of terrestrial ecosystem carbon accumulation for the past century, which was especially pronounced at high latitudes. This underestimation is equivalent to 45% of the total carbon emissions (164 Pg C) caused by global land use change at the same time. Our analyses highlight the need to constrain ecosystem models using observation-based and locally adapted R_h values to obtain reliable predictions of the carbon sink capacity of terrestrial ecosystems.