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Abstract:
A consistent, process-based methane module for a global land surface scheme has been
developed which is general enough to be applied in permafrost regions as well as wetlands outside
permafrost areas. Methane production, oxidation and transport by ebullition, diffusion and plants
are represented. Oxygen has been explicitly incorporated in diffusion, transport by plants and two
5 oxidation processes, of which one uses soil oxygen, while the other uses oxygen that is available
via roots. Permafrost and wetland soils show special behaviour, such as variable soil pore space due
to freezing and thawing or water table depths due to changing soil water content. This has been
integrated directly into the methane-related processes. A detailed application at the polygonal tundra
site Samoylov, Lena delta, Russia, is used for evaluation purposes. The application at Samoylov also
10 shows differences in the importance of the several transport processes and in the methane dynamics
under varying soil moisture, ice and temperature conditions during different seasons and on different
microsites. These microsites are the elevated moist polygonal rim and the depressed wet polygonal
center. The evaluation shows sufficiently good agreement with field observations despite the fact that
the module has not been specifically calibrated to these data.