Northern peatlands have cooled the global climate by accumulating large quantities of soil
carbon (C) over thousands of years. Maintaining the C sink function of these peatlands and …

Climate change interacts with the sources and cycling of contaminants, such as
radionuclides, in the environment. In this review, we discuss the implications of climate …

High-latitude peatlands are changing rapidly in response to climate change, including
permafrost thaw. Here, we reconstruct hydrological conditions since the seventeenth century …

Northern peatlands are a major component of the global carbon (C) cycle. Widespread
climate‐driven ecohydrological changes in these ecosystems can have major …

Under a pronounced climate warming, permafrost has been degrading in most areas
globally, but it is still unclear in the northwestern part of the Da Xing'anling Mountains …

The fate of the carbon stored in frozen peatlands in Canada's Hudson Bay Lowlands (HBL)
depends strongly on water, with wetter conditions favoring long-term storage. Dynamic …

Climate warming is leading to permafrost thaw in northern peatlands, and current
predictions suggest that thawing will drive greater surface wetness and an increase in …

Methane (CH4) emissions from northern peatlands are projected to increase due to climate
change, primarily because of projected increases in soil temperature. Yet, the rates and …

The anthropogenic climate change threatens northern permafrost environments. This
compromises the existence of permafrost landforms, such as palsas and peat plateaus …

Permafrost peatlands are vulnerable to rapid structural changes under climatic warming,
including vertical collapse. Peatland water budgets, and therefore peat hydraulic properties …