The physical and chemical changes that accompany permafrost thaw directly influence the
microbial communities that mediate the decomposition of formerly frozen organic matter …

The priming effect (PE) is the short-term increase or decrease in the rate of soil organic
matter mineralization in response to a stimulus, such as the addition of carbon (C) and/or …

Arctic wetlands are known methane (CH4) emitters but recent studies suggest that the Arctic
CH4 sink strength may be underestimated. Here we explore the capacity of well-drained …

Permafrost underlies approximately one quarter of Northern Hemisphere terrestrial surfaces
and contains 25–50% of the global soil carbon (C) pool. Permafrost soils and the C stocks …

Biogeochemical cycling in permafrost‐affected ecosystems remains associated with large
uncertainties, which could impact the Earth's greenhouse gas budget and future climate …

Nitrogen regulates multiple aspects of the permafrost climate feedback, including plant
growth, organic matter decomposition, and the production of the potent greenhouse gas …

Since the start of the Anthropocene, northern seasonally frozen peatlands have been
warming at a rate of 0.6° C per decade, twice that of the Earth's average rate, thereby …

The northern permafrost region has been projected to shift from a net sink to a net source of
carbon under global warming. However, estimates of the contemporary net greenhouse gas …

Nitrous oxide (N 2 O) is a long-lived potent greenhouse gas and stratospheric ozone-
depleting substance, which has been accumulating in the atmosphere since the pre …

In the context of climate change, research on frozen soils has attracted much attention in
recent years, and numerous research papers have been published on these topics in the …