Methane emissions from subtaiga mires of Western Siberia: The “standard model” Bc5

The impact of permafrost on carbon dioxide and methane fluxes in Siberia: A meta-analysis

There are serious concerns associated with greenhouse gases (GHG) fluxes in high latitude ecosystems and how the permafrost thawing may potentially affect the global climate, through the alteration of carbon (C) dioxide (CO₂) and methane (CH₄) emissions. We performed a meta-analysis of 3002 observations from 104 published studies on CO₂ and CH₄ fluxes in Siberia (Russian Federation). Siberia is a vast region characterized by a large C-rich permafrost region, which is already degrading due to escalating climate change, and also large wetland areas, also regarded as a source of CH₄. GHG fluxes were strongly controlled by location (Western, Central, Eastern, and Far East Siberia), permafrost presence and season. Maximum CO₂ fluxes, in the permafrost zone, were observed in Central and Eastern Siberia. In the non-permafrost zone, maximum CO₂ fluxes were found in Western Siberia. According to our analyses, CH₄ fluxes in the permafrost zone were significantly different in all parts of Siberia. Thus, permafrost has a more profound effect on CH₄ than on CO₂ flux. The rank order of increase of CH₄ emissions among the various Siberian regions is as follows: Central < Eastern < Western < Far East. In the non-permafrost area, CH₄ fluxes in Western Siberia are higher than those in the Central part. Soil temperature was the only significant predictor of soil CO₂ flux in the permafrost area. CH₄ fluxes were well correlated with temperature and soil water content in the permafrost zone, but only dependent on temperature in the non-permafrost area. In this meta-analysis, we established several statistically significant temporal trends of long-term changes of GHG fluxes over three decades (1984-2017): an increasing trend of soil CO₂ fluxes in the non-permafrost area of Western Siberia and a declining trend in the non-permafrost area of Central Siberia. There was also a significant increasing trend of CH₄ fluxes in the permafrost area of Eastern Siberia, and its decreasing trend in the non-permafrost area of Western Siberia.