Methane Flux From Arctic Tundras: It's The Hydrology, Stupid!

Methane fluxes from the arctic permafrost areas attract scientific attention because the release of this powerful greenhouse gas may act as a positive feedback to climate warming. Methane release, generally, is enhanced by increasing the metabolic activity of methane bacteria in warmer arctic soils, or by the release of methane from melting permafrost.

However, research in the Northeast Siberian tundra has shown the importance of floodplain hydrology. The floodplains of arctic lowland rivers are major methane sources, where methane fluxes may be 5 times as high as in non-flooded tundra bogs. Moreover, these fluxes are very sensitive to river discharge fluctuations and the incidence of river floods. During a two year field campaign the drier year resulted in a 75% reduction of the methane flux. Currently, both air temperature and river discharges are rising significantly in the arctic.

Oral Presentation: Ko Van Huissteden, Dolaman, A.J., Maximov, T.C. Floodplain hydrology and spatial/temporal variation of methane fluxes inarctic tundra, North East Siberia.