Ecosystem scale methane fluxes in a natural temperate bog-pine forest in southern Germany

•Natural, temperate bog-pine ecosystem is a CO2 sink but a small source of CH4.•Overall, the ecosystem is a small net annual greenhouse gas sink.•At high water levels, methane fluxes correlate best with air temperature. Methane (CH4) and carbon dioxide (CO2) exchange were investigated over 15 months...

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Veröffentlicht in:Agricultural and forest meteorology 2014-11, Vol.198-199, p.273-284
Hauptverfasser: Hommeltenberg, Janina, Mauder, Matthias, Drösler, Matthias, Heidbach, Katja, Werle, Peter, Schmid, Hans Peter
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Sprache:eng
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Zusammenfassung:•Natural, temperate bog-pine ecosystem is a CO2 sink but a small source of CH4.•Overall, the ecosystem is a small net annual greenhouse gas sink.•At high water levels, methane fluxes correlate best with air temperature. Methane (CH4) and carbon dioxide (CO2) exchange were investigated over 15 months above a natural bog-pine site in the pre-alpine region of southern Germany. The measurements indicate annual methane emissions of +5.3±0.34gCm−2a−1 and an annual CO2 uptake of −62±20gCm−2a−1, resulting in a global warming potential balance of −50±74g [CO2 eq.]m−2a−1. Air temperature was identified as the environmental parameter showing the highest correlation with methane production, except for periods with low water table (
ISSN:0168-1923
1873-2240
DOI:10.1016/j.agrformet.2014.08.017