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AGU: Geophysical Research Letters

 

Index Terms

  • Atmospheric Composition and Structure: Biosphere/atmosphere interactions
  • Biogeosciences: Carbon cycling
  • Biogeosciences: Diel, seasonal, and annual cycles
  • Biogeosciences: Wetlands

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 32, L23804, 4 PP., 2005
doi:10.1029/2005GL024731

An Atlantic blanket bog is a modest CO2 sink

Matteo Sottocornola

Department of Civil and Environmental Engineering, University College Cork, Cork, Ireland

Ger Kiely

Department of Civil and Environmental Engineering, University College Cork, Cork, Ireland

Northern peatlands contain 1/3 of the world's soil carbon pool. Blanket bogs are peatlands that occur in maritime regions where precipitation is much greater than evapotranspiration. The role of blanket bogs in C dynamics has not been quantified. We describe an investigation of CO2 fluxes using an eddy covariance (EC) system in a pristine Atlantic blanket bog in Ireland during 2003 and 2004. This is the first multiyear study using EC techniques in a blanket bog. We found that the bog ecosystem was a CO2 sink for five months in each year. The annual CO2 flux had a sink magnitude of −49 (2003) and −61 g C m−2 (2004). These magnitudes are similar to boreal raised bogs, while higher values have been reported for boreal fens and lower for subarctic fens.

Received 22 September 2005; accepted 28 October 2005; published 2 December 2005.

Citation: Sottocornola, M., and G. Kiely (2005), An Atlantic blanket bog is a modest CO2 sink, Geophys. Res. Lett., 32, L23804, doi:10.1029/2005GL024731.

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