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 uptake will respond to ongoing climate change. In particular, the soil-to-atmosphere CO2 flux, commonly though imprecisely termed soil respiration (RS ), is one of the largest carbon fluxes in the Earth system. An increasing number of high-frequency RS measurements (typically, from an automated system with hourly sampling) have been made over the last two decades; an increasing number of methane measurements are being made with such systems as well. Such high frequency data are an invaluable resource for understanding GHG fluxes, but lack a central database or repository...
Field observations of the soil-to-atmosphere CO2 flux—soil respiration, RS—are a prime example of ‘l...
Field observations of the soil-to-atmosphere CO2 flux—soil respiration, RS—are a prime example of ‘l...
Soil respiration, the flux of CO<sub>2</sub> from the soil to the atmosphere represents a major flux...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Field observations of the soil-to-atmosphere CO2 flux—soil respiration, RS—are a prime example of ‘l...
Field observations of the soil-to-atmosphere CO2 flux—soil respiration, RS—are a prime example of ‘l...
Field observations of the soil-to-atmosphere CO2 flux—soil respiration, RS—are a prime example of ‘l...
Soil respiration, the flux of CO<sub>2</sub> from the soil to the atmosphere represents a major flux...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Globally, soils store two to three times as much carbon as currently resides in the atmosphere, and ...
Field observations of the soil-to-atmosphere CO2 flux—soil respiration, RS—are a prime example of ‘l...
Field observations of the soil-to-atmosphere CO2 flux—soil respiration, RS—are a prime example of ‘l...
Field observations of the soil-to-atmosphere CO2 flux—soil respiration, RS—are a prime example of ‘l...
Soil respiration, the flux of CO<sub>2</sub> from the soil to the atmosphere represents a major flux...