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Modeling the spatio-temporal variability in subsurface thermal regimes across a low-relief polygonal tundra landscape
2016
The Cryosphere Discussions
Vast carbon stocks stored in permafrost soils of Arctic tundra are under risk of release to atmosphere under warming climate. Ice-wedge polygons in the low-gradient polygonal tundra create a complex mosaic of microtopographic features. The microtopography plays a critical role in regulating the fine scale variability in thermal and hydrological regimes in the polygonal tundra landscape underlain by continuous permafrost. Modeling of thermal regimes of this sensitive ecosystem is essential for
doi:10.5194/tc-2016-29
fatcat:65deoq73gnegbgmikoedx5kxv4