Soil respiration (Rs), the soil‐to‐atmosphere CO2 flux produced by microbes and plant
roots, is a critical but uncertain component of the global carbon cycle. Our current …

Soil respiration (Rs), the efflux of CO2 from soils to the atmosphere, is a major component of
the terrestrial carbon cycle, but is poorly constrained from regional to global scales. The …

Quantifying global soil respiration (RSG) and its response to temperature change are critical
for predicting the turnover of terrestrial carbon stocks and their feedbacks to climate change …

Soil respiration (Rs) is a major pathway by which fixed carbon in the biosphere is returned to
the atmosphere, yet there are limits to our ability to predict respiration rates using …

To develop a model describing the dependence of annual soil respiration on climate and
soil properties, we compiled 657 published annual soil respiration (Rs) measurements that …

Soil respiration (Rs; the soil surface‐to‐atmosphere CO2 flux) has been measured in the
field for decades, but only recently have we begun to assemble and leverage these small …

The flux of carbon dioxide from the soil to the atmosphere (soil respiration) is one of the
major fluxes in the global carbon cycle. At present, the accumulated field observation data …

Biome‐specific soil respiration (Rs) has important yet different roles in both the carbon cycle
and climate change from regional to global scales. To date, no comparable studies related …

Soil microbial respiration (Rh) is a large but uncertain component of the terrestrial carbon
cycle. Carbon–climate feedbacks associated with changes to Rh are likely, but Rh …

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 …