Soil respiration (Rs), the soil‐to‐atmosphere flux of CO2, is a dominant but uncertain part of
the carbon cycle, even after decades of study. This review focuses on progress in …

The net ecosystem exchange (NEE) is the difference between ecosystem CO 2 assimilation
and CO 2 losses to the atmosphere. Ecosystem respiration (R eco), the efflux of CO 2 from …

Terrestrial enhanced weathering (EW) through the application of Mg‐or Ca‐rich rock dust to
soil is a negative emission technology with the potential to address impacts of climate …

Belowground carbon (C) dynamics of terrestrial ecosystems play an important role in the
global C cycle and thereby in climate regulation. Globally, land-use change is a major driver …

Globally, soils store two to three times as much carbon as currently resides in the
atmosphere, and it is critical to understand how soil greenhouse gas (GHG) emissions and …

Background An acceleration of model-data synthesis activities has leveraged many
terrestrial carbon datasets, but utilization of soil respiration (RS) data has not kept pace …

Soil respiration, defined as the total flux of carbon dioxide (CO 2) from the soil to the
atmosphere, is a key ecosystem process that affects the regional and global carbon (C) …

Wetlands store a disproportionately large fraction of organic carbon relative to their areal
coverage, and thus play an important role in global climate mitigation. As destabilization of …

Intensification, the process of intensifying land management to enhance agricultural goods,
results in “intensive” pastures that are planted with productive grasses and fertilized. These …

Wetlands play an important role in reducing global warming potential in response to global
climate change. Unfortunately, due to the effects of human disturbance and natural erosion …