66 research outputs found
Quantifying landscape-level methane fluxes in subarctic Finland using a multiscale approach
Journal ArticleQuantifying landscape-scale methane (CH4) fluxes from boreal and arctic regions, and determining how they are controlled, is critical for predicting the magnitude of any CH4 emission feedback to climate change. Furthermore, there remains uncertainty regarding the relative importance of small areas of strong methanogenic activity, vs. larger areas with net CH4 uptake, in controlling landscape-level fluxes. We measured CH4 fluxes from multiple microtopographical subunits (sedge-dominated lawns, interhummocks and hummocks) within an aapa mire in subarctic Finland, as well as in drier ecosystems present in the wider landscape, lichen heath and mountain birch forest. An intercomparison was carried out between fluxes measured using static chambers, up-scaled using a high-resolution landcover map derived from aerial photography and eddy covariance. Strong agreement was observed between the two methodologies, with emission rates greatest in lawns. CH4 fluxes from lawns were strongly related to seasonal fluctuations in temperature, but their floating nature meant that water-table depth was not a key factor in controlling CH4 release. In contrast, chamber measurements identified net CH4 uptake in birch forest soils. An intercomparison between the aerial photography and satellite remote sensing demonstrated that quantifying the distribution of the key CH4 emitting and consuming plant communities was possible from satellite, allowing fluxes to be scaled up to a 100 km2 area. For the full growing season (May to October), ~ 1.1-1.4 g CH4 m-2 was released across the 100 km2 area. This was based on up-scaled lawn emissions of 1.2-1.5 g CH4 m-2, vs. an up-scaled uptake of 0.07-0.15 g CH4 m-2 by the wider landscape. Given the strong temperature sensitivity of the dominant lawn fluxes, and the fact that lawns are unlikely to dry out, climate warming may substantially increase CH4 emissions in northern Finland, and in aapa mire regions in general.This work was carried out within the Natural Environment
Research Council (NERC) funded Arctic Biosphere Atmosphere
Coupling at Multiple Scales (ABACUS) project (a contribution
to International Polar Year 2007_2008) plus NERC small grant
NE/F010222/1 awarded to RB and BH. We are grateful for the support of the staff at the Kevo Subarctic Research Institute, to
David Sayer for operation and maintenance of the eddy covariance
apparatus, and to Lorna English for helping with the
analysis of the CH4 samples. We also thank the NERC Field
Spectroscopy Facility for support in ground data collection for
the remote sensing analysis. Finally, we wish to express our
gratitude to two anonymous reviewers whose comments and
suggestions substantially improved the manuscript
Evidence for nitrogen accumulation: the total nitrogen budget of the terrestrial biosphere of a lowland agricultural catchment
Chemical characteristics of particulate organic matter from a small, mountainous river system in the Oregon Coast Range, USA
The interactive effects of excess reactive nitrogen and climate change on aquatic ecosystems and water resources of the United States
Comment on “Burt T., Worrall F. 2007. Non-stationarity in long time series: some curious reversals in the memory effect
Spatio-temporal trends in Nitrate concentrations in groundwater-dominated Chalk streams, Dorset (UK)
Temporal and spatial analysis of nitrate concentrations from the Frome and Piddle catchments in Dorset (UK) for water years 1978 to 2007: Evidence for nitrate breakthrough?
Statistical analysis of nitrate concentrations from the Rivers Frome and piddle (Dorset, UK) for the period 1965-2007
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