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

Abstract Quantifying landscape‐scale methane (CH 4) fluxes from boreal and arctic regions, and determining how they are controlled, is critical for predicting the magnitude of any CH 4 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 CH 4 uptake, in controlling landscape‐level fluxes. We measured CH 4 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. CH 4 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 CH 4 release. In contrast, chamber measurements identified net CH 4 uptake in birch forest soils. An intercomparison between the aerial photography and satellite remote sensing demonstrated that quantifying the distribution of the key CH 4 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 CH 4 m−2 was released across the 100 km2 area. This was based on up‐scaled lawn emissions of 1.2–1.5 g CH 4 m−2, vs. an up‐scaled uptake of 0.07–0.15 g CH 4 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 CH 4 emissions in northern Finland, and in aapa mire regions in general.

[1]  M. Jorgenson,et al.  Erratum: Effect of permafrost thaw on CO2 and CH4 exchange in a western Alaska peatland chronosequence (2013 Environ. Res. Lett. 9 085004) , 2014 .

[2]  W. Oechel,et al.  Spatial variation in landscape‐level CO2 and CH4 fluxes from arctic coastal tundra: influence from vegetation, wetness, and the thaw lake cycle , 2013, Global change biology.

[3]  C. Curry The consumption of atmospheric methane by soil in a simulated future climate , 2009 .

[4]  C. Tucker,et al.  Dynamics of aboveground phytomass of the circumpolar Arctic tundra during the past three decades , 2012 .

[5]  P. Crill,et al.  Environmental and physical controls on northern terrestrial methane emissions across permafrost zones , 2013, Global Change Biology.

[6]  R. Macdonald,et al.  Sensitivity of the carbon cycle in the Arctic to climate change , 2009 .

[7]  S. Juutinen,et al.  Methane dynamics in different boreal lake types , 2009 .

[8]  Corinne Le Quéré,et al.  Carbon and Other Biogeochemical Cycles , 2014 .

[9]  Wataru Takeuchi,et al.  Estimation of methane emission from West Siberian wetland by scaling technique between NOAA AVHRR and SPOT HRV , 2003 .

[10]  Peter M. Cox,et al.  Climate feedback from wetland methane emissions , 2004 .

[11]  M. Wilmking,et al.  Do we miss the hot spots? – The use of very high resolution aerial photographs to quantify carbon fluxes in peatlands , 2008 .

[12]  Drew T. Shindell,et al.  Impacts of climate change on methane emissions from wetlands , 2004 .

[13]  M. Jorgenson,et al.  Effect of permafrost thaw on CO2 and CH4 exchange in a western Alaska peatland chronosequence , 2014 .

[14]  Patrick M. Crill,et al.  Freshwater Methane Emissions Offset the Continental Carbon Sink , 2011, Science.

[15]  P. Roger,et al.  Production, oxidation, emission and consumption of methane by soils: A review , 2001 .

[16]  D. Pennock,et al.  Methane and nitrous oxide emissions from mature forest stands in the boreal forest, Saskatchewan, Canada , 2009 .

[17]  S. Haapanala,et al.  Spatial variation in plant community functions regulates carbon gas dynamics in a boreal fen ecosystem , 2007 .

[18]  A. Dolman,et al.  Multi-technique assessment of spatial and temporal variability of methane fluxes in a peat meadow , 2010 .

[19]  O. T. Denmead,et al.  Approaches to measuring fluxes of methane and nitrous oxide between landscapes and the atmosphere , 2008, Plant and Soil.

[20]  L. Verchot,et al.  A global inventory of the soil CH4 sink , 2007 .

[21]  S. Sjögersten,et al.  Depth Distribution of Net Methanotrophic Activity at a Mountain Birch Forest—Tundra Heath Ecotone, Northern Sweden , 2007 .

[22]  R. Kormann,et al.  An Analytical Footprint Model For Non-Neutral Stratification , 2001 .

[23]  Paul L. G. Vlek,et al.  An appraisal of global wetland area and its organic carbon stock , 2005 .

[24]  P. Martikainen,et al.  Factors controlling large scale variations in methane emissions from wetlands , 2003 .

[25]  A. J. Dolman,et al.  Spatial and temporal dynamics in eddy covariance observations of methane fluxes at a tundra site in Northeastern Siberia , 2011 .

[26]  Stephen Sitch,et al.  Numerical Terradynamic Simulation Group 1-2007 ASSESSING THE CARBON BALANCE OF CIRCUMPOLAR ARCTIC TUNDRA USING REMOTE SENSING AND PROCESS MODELING , 2018 .

[27]  Andrei P. Sokolov,et al.  Rising methane emissions in response to climate change in Northern Eurasia during the 21st century , 2011 .

[28]  D. Davydov,et al.  Annual variation of CH4 emissions from the middle taiga in West Siberian Lowland (2005–2009): a case of high CH4 flux and precipitation rate in the summer of 2007 , 2012 .

[29]  T. Riutta,et al.  Annual cycle of methane emission from a boreal fen measured by the eddy covariance technique , 2007 .

[30]  Qianlai Zhuang,et al.  Methane emissions from wetlands: biogeochemical, microbial, and modeling perspectives from local to global scales , 2013, Global change biology.

[31]  P. Ciais,et al.  Permafrost carbon-climate feedbacks accelerate global warming , 2011, Proceedings of the National Academy of Sciences.

[32]  Jeffrey R. White,et al.  A synthesis of methane emissions from 71 northern, temperate, and subtropical wetlands , 2014, Global change biology.

[33]  K. Bäckstrand,et al.  Annual cycle of methane emission from a subarctic peatland , 2010 .

[34]  Jukka Turunen,et al.  Estimating carbon accumulation rates of undrained mires in Finland–application to boreal and subarctic regions , 2002 .

[35]  J. Heikkinen,et al.  Carbon dioxide and methane dynamics in a sub-Arctic peatland in northern Finland , 2002 .

[36]  P. Crill,et al.  A catchment-scale carbon and greenhouse gas budget of a subarctic landscape , 2007, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.

[37]  Robert J. Evans,et al.  The disappearance of relict permafrost in boreal north America: Effects on peatland carbon storage and fluxes , 2007 .