Predicting long-term carbon mineralization and trace gas production from thawing permafrost of Northeast Siberia

Author:

Knoblauch Christian1,Beer Christian2,Sosnin Alexander3,Wagner Dirk4,Pfeiffer Eva-Maria1

Affiliation:

1. University of Hamburg; Institute of Soil Science; KlimaCampus, Allende-Platz 2; 20146; Hamburg; Germany

2. Max Planck Institute for Biogeochemistry; Hans-Knöll-Str. 10; 07745; Jena; Germany

3. Faculty of Geography and Geoecology; University of St. Petersburg; 33, 10th line; 199178; St. Petersburg; Russia

4. Helmholtz Centre Potsdam; GFZ German Research Centre for Geosciences; Section 4.5 Geomicrobiology; Telegrafenberg; 14473; Potsdam; Germany

Publisher

Wiley

Subject

General Environmental Science,Ecology,Environmental Chemistry,Global and Planetary Change

Reference49 articles.

1. ICBM: the introductory carbon balance model for exploration of soil carbon balances;Andrén;Ecological Applications,1997

2. Potential feedback of thawing permafrost to the global climate system through methane emission;Anisimov;Environmental Research Letters,2007

3. The timing of snow melt controls the annual CO2 balance in a subarctic fen;Aurela;Geophysical Research Letters,2004

4. Effects of soil freezing and thawing on vegetation carbon density in Siberia: a modeling analysis with the Lund-Potsdam-Jena Dynamic Global Vegetation Model (LPJ-DGVM);Beer;Global Biogeochemical Cycles,2007

5. Response of methanogenic archaea to Late Pleistocene and Holocene climate changes in the Siberian Arctic;Bischoff;Global Biogeochemical Cycles

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