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  Process-based modelling of the methane balance in periglacial landscapes (JSBACH-methane)

Kaiser, S., Göckede, M., Castro-Morales, K., Knoblauch, C., Ekici, A., Kleinen, T., et al. (2017). Process-based modelling of the methane balance in periglacial landscapes (JSBACH-methane). Geoscientific Model Development, 10(1), 333-358. doi:10.5194/gmd-10-333-2017.

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BGC2471D.pdf (Verlagsversion), 3MB
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http://dx.doi.org/10.5194/gmd-10-333-2017 (Verlagsversion)
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 Urheber:
Kaiser, Sonja1, Autor           
Göckede, Mathias2, Autor           
Castro-Morales, Karel2, Autor           
Knoblauch, C., Autor
Ekici, Altug1, Autor           
Kleinen, T., Autor
Zubrzycki, S., Autor
Sachs, T., Autor
Wille, C., Autor
Beer, C., Autor
Affiliations:
1Department Biogeochemical Systems, Prof. M. Heimann, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497755              
2Integrating surface-atmosphere Exchange Processes Across Scales - Modeling and Monitoring, Dr. Mathias Göckede, Department Biogeochemical Systems, Prof. M. Heimann, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1938313              

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 Zusammenfassung: 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.

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 Datum: 2016-12-052017-01-242017-01-24
 Publikationsstatus: Erschienen
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 Identifikatoren: Anderer: BGC2471
DOI: 10.5194/gmd-10-333-2017
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Titel: Geoscientific Model Development
  Andere : Geosci. Model Dev.
  Kurztitel : GMD
Genre der Quelle: Zeitschrift
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Affiliations:
Ort, Verlag, Ausgabe: Göttingen : Copernicus Publ.
Seiten: - Band / Heft: 10 (1) Artikelnummer: - Start- / Endseite: 333 - 358 Identifikator: ISSN: 1991-959X
CoNE: https://pure.mpg.de/cone/journals/resource/1991-959X