4.5 Article

A multisite analysis of temporal random errors in soil CO2 efflux

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES
Volume 120, Issue 4, Pages 737-751

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1002/2014JG002690

Keywords

uncertainty; soil respiration; ecosystem fluxes; allometric scaling; soil moisture; measurement error

Funding

  1. University of Delaware by CONACyT [CVU 397284]
  2. Austrian Science Fund (FWF) [P18756-B16, P22214-B17]
  3. DOE University-Lab EPSCoR [DE-FG02-08ER46506]
  4. DOE BER [DE-SC0008088]
  5. Sevilleta LTER
  6. Academy of Finland [218094, 213093]
  7. Academy of Finland Finnish Centre of Excellence Program
  8. CONACyT [Ciencia Basica-152671]
  9. NASA [NNX13AQ06G]
  10. USDA [2014-67003-22070]
  11. U.S. Department of Energy (DOE) [DE-SC0008088] Funding Source: U.S. Department of Energy (DOE)
  12. Austrian Science Fund (FWF) [P18756] Funding Source: Austrian Science Fund (FWF)
  13. Direct For Biological Sciences
  14. Division Of Environmental Biology [1440478] Funding Source: National Science Foundation

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An important component of the terrestrial carbon balance is the efflux of CO2 from soils to the atmosphere, which is strongly influenced by changes in soil moisture and temperature. Continuous measurements of soil CO2 efflux are available around the world, and there is a need to develop and improve analyses to better quantify the precision of the measurements. We focused on random errors in measurements, which are caused by unknown and unpredictable changes such as fluctuating environmental conditions. We used the CO2 gradient flux method with two different algorithms to study the temporal variation of soil CO2 efflux and associated random errors at four different ecosystems with wide ranges in mean annual temperature, soil moisture, and soil CO2 efflux. Our results show that random errors were better explained by a double-exponential distribution, had a mean value close to zero, were nonheteroscedastic, and were independent of soil moisture conditions. Random errors increased with the magnitude of soil CO2 efflux and scale isometrically (scaling exponent approximate to 1) within and across all sites, with a single relation common to all data. This isometric scaling is unaffected by ecosystem type, soil moisture conditions, and soil CO2 efflux range (maximum and minimum values within an ecosystem). These results suggest larger uncertainty under extreme events that increase soil CO2 efflux rates. The accumulated annual uncertainty due to random errors varied between 0.38 and 2.39%. These results provide insights on the scalability of the sensitivity of soil CO2 efflux to changing weather conditions across ecosystems.

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