Working Group of the Arctic Council
Figure 8.4 Mechanisms by which carbon may be lost from Arctic soils in permafrost areas (excluding fire). Area 1 has a spatially homogenous increase in active layer thickness and Area 2 has spatially heterogeneous permafrost thaw driven by differences in soil ice content (after van Huissteden and Dolman, 2013).
Meta Data
Publication:
Snow, Water, Ice and Permafrost in the Arctic (SWIPA) 2017
Page number:
208
Type:
Schematic
Caption:
Figure 8.4 Mechanisms by which carbon may be lost from Arctic soils in permafrost areas (excluding fire). Area 1 has a spatially homogenous increase in active layer thickness and Area 2 has spatially heterogeneous permafrost thaw driven by differences in soil ice content (after van Huissteden and Dolman, 2013).
Copyright:
Arctic Monitoring and Assessment Programme (AMAP)
Cartographer / Designer:
Burnthebook.co.uk