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

Reanalysis data show an increasing trend in Arctic precipitation over the 20th century, but
changes are not homogenous across seasons or space. The observed hydroclimate …

Peatlands within the northern permafrost region cover approximately 2 million km2 and are
characterized by organic soils that can be several meters thick, and a fine-scale mosaic of …

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

Northern boreal peatlands are important ecosystems in modulating global biogeochemical
cycles, yet their biological communities and related carbon dynamics are highly sensitive to …

Permafrost peatlands are found in high-latitude regions and store globally-important
amounts of soil organic carbon. These regions are warming at over twice the global average …

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 …

In this study, we investigated the links between peat carbon accumulation and past
ecological and hydrological conditions in three peatlands (Bouleau, Mista, Auassat) which …

Northern peatlands have accumulated large carbon (C) stocks since the last deglaciation
and during past millennia they have acted as important atmospheric C sinks. However, it is …