While heterotrophic respiration (Rh) makes up about a quarter of gross global terrestrial
carbon fluxes, it remains among the least-observed carbon fluxes, particularly outside the …

Soil heterotrophic respiration (SHR) is important for carbon‐climate feedbacks because of its
sensitivity to soil carbon, climatic conditions and nutrient availability. However, available …

On regional to global scales, few constraints exist on gross primary productivity (GPP) and
ecosystem respiration (R e) fluxes. Yet constraints on these fluxes are critical for evaluating …

A better understanding of the local variability in land‐atmosphere carbon fluxes is crucial to
improving the accuracy of global carbon budgets. Operational satellite data backed by …

Soil respiration–RS, the flux of CO 2 from the soil to the atmosphere–is probably the least
well constrained component of the terrestrial carbon cycle. Here we introduce the SRDB …

Soil heterotrophic respiration (RH) is one of the largest and most uncertain components of
the terrestrial carbon cycle, directly reflecting carbon loss from soils to the atmosphere …

Soil heterotrophic respiration (Rh) 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 …

This paper combines an atmospheric transport model and a terrestrial ecosystem model to
estimate gross primary productivity (GPP) and net ecosystem productivity (NEP) of the land …

Global soils store at least twice as much carbon as Earth's atmosphere,. The global soil-to-
atmosphere (or total soil respiration, RS) carbon dioxide (CO2) flux is increasing,, but the …

Terrestrial ecosystem respiration (R eco) represents a large carbon source from land to
atmosphere and is highly spatiotemporally heterogeneous across scales. Upscaling of field …