Long winters and permafrost in Alaskan boreal forests inhibits the decomposition of organic materials, promoting accrual as a surface soil organic lay...

Understanding the carbon-climate feedback during past abrupt climate transitions is important for contextualizing future permafrost stability and asso...

Permafrost underlies 24% of the land surface in the northern hemisphere and stores about 3 times the amount of carbon in earths atmosphere. Climate-in...

Rapid Arctic warming is thawing carbon-rich permafrost, releasing greenhouse gasses to the atmosphere and accelerating global climate change. Despite ...

There is great uncertainty surrounding the permafrost carbon feedback from Arctic soils throughout the depth profile under abrupt thaw. Soil in the ac...

The active layer in permafrost terrain is the soil horizon above multi-year frozen ground that undergoes seasonal freeze-thaw cycles. Increases in act...

Cross-scale feedbacks between ecohydrology, permafrost thaw, and wildfire will dictate the future structure and function of northern peatlands, which ...