- 1Pioneer Center Land-Craft, Aarhus University, Aarhus, Denmark (claire.treat@agro.au.dk)
- 2Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Potsdam, Germany
Cold season processes and emissions can be critical for determining annual budgets of CO2 and methane (CH4) in Arctic and other high-latitude ecosystems but there are relatively few measurements of winter fluxes and corresponding soil processes. In this talk, we will present results from investigating seasonality in greenhouse gas fluxes and processes controlling them, with a special emphasis on CH4 emissions from a boreal peatland. We measured CO2, CH4, and N2O fluxes for more than a year from an upland forest, dry bog, and wet bog at a site in boreal Finland using automated and manual chambers. Net CO2 uptake and CH4 emissions were highest in summer while N2O fluxes were nearly always below detection. Plant transport and oxidation of CH4 played an important role in CH4 fluxes during the summer as well as into the fall. CH4 emissions were enhanced throughout the fall due to plant transport and showed little seasonality in the fall in drier bog microtopographies. Net CO2 and CH4 emissions from the wet bog continued into December until snowpack formation, which led to an icy layer at the top of the peat profile. In the spring as snow melted and soils thawed, we saw an emissions pulse of CH4. Additional measurements showed the highest concentrations of CH4 in the peat porewater in the spring, indicating the accumulation of microbially-produced CH4 in the unfrozen peat under the snowpack during the winter. Furthermore, potential decomposition in Sphagnum peat showed little temperature sensitivity in laboratory experiments, indicating microbial adaptation to cold temperatures not seen in the dry bog or upland forest soils. Sustained biological activity in peat can continue at low temperatures over winter and lead to substantial enhancements in CH4 and CO2 emissions, although the timing of emissions is controlled by interactions in physical environment: snow melt, soil thawing, and plant-mediated transport.
How to cite: Treat, C. C., Jentzsch, K., van Delden, L., Hashemi, J., and Baysinger, M.: CO2 and CH4 fluxes and processes in a boreal bog and surroundings: a chilling tale of cold-season greenhouse gas emissions, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-3746, https://doi.org/10.5194/egusphere-egu25-3746, 2025.