Quantifying landscape-level methane fluxes in subarctic Finland using a multiscale approach

Iain P. Hartley, Timothy C. Hill, Thomas J. Wade, Robert J. Clement, John B. Moncrieff, Ana Prieto-Blanco, Mathias I. Disney, Brian Huntley, Mathew Williams, Nicholas J K Howden, Philip A. Wookey, Robert Baxter

    Research output: Contribution to journalArticle

    16 Citations (Scopus)
    38 Downloads (Pure)

    Abstract

    Quantifying 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 m2 was released across the 100 km2 area. This was based on up-scaled lawn emissions of 1.2–1.5 g CH4 m2 , vs. an up-scaled uptake of 0.07–0.15 g CH4 m2 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.
    Original languageEnglish
    Pages (from-to)3712-3725
    Number of pages14
    JournalGlobal Change Biology
    Volume21
    Issue number10
    Early online date17 Jun 2015
    DOIs
    Publication statusPublished - 27 Jun 2015

    Keywords

    • Aapa mire
    • Arctic
    • Climate change
    • Eddy covariance
    • Methane oxidation
    • Methanogenesis
    • Remote sensing
    • Static chambers

    ASJC Scopus subject areas

    • Ecology
    • Global and Planetary Change
    • Environmental Science(all)
    • Environmental Chemistry

    Fingerprint Dive into the research topics of 'Quantifying landscape-level methane fluxes in subarctic Finland using a multiscale approach'. Together they form a unique fingerprint.

  • Cite this

    Hartley, I. P., Hill, T. C., Wade, T. J., Clement, R. J., Moncrieff, J. B., Prieto-Blanco, A., Disney, M. I., Huntley, B., Williams, M., Howden, N. J. K., Wookey, P. A., & Baxter, R. (2015). Quantifying landscape-level methane fluxes in subarctic Finland using a multiscale approach. Global Change Biology, 21(10), 3712-3725. https://doi.org/10.1111/gcb.12975