Methane (CH4) is produced in many natural systems that are vulnerable to change under a
warming climate, yet current CH4 budgets, as well as future shifts in CH4 emissions, have …

The rewetting of dry soils and the thawing of frozen soils are short-term, transitional
phenomena in terms of hydrology and the thermodynamics of soil systems. The impact of …

Wildfires are a pervasive disturbance in boreal forests, and the frequency and intensity of
boreal wildfires is expected to increase with climate warming. Boreal forests store a large …

It is widely recognized that forest soils are important terrestrial sinks for atmospheric CH 4;
however, the complexity of the underlying microbial production and oxidation processes …

This study investigated the relationship between climate and landscape characteristics and
surface fuel consumption as well as the effects of variations in postfire organic layer depth …

Wildfires strongly regulate carbon (C) cycling and storage in boreal forests and account for
almost 10% of global fire C emissions. However, the anticipated effects of climate change on …

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 …

Worldwide, regularly recurring wildfires shape many peatland ecosystems to the extent that
fire‐adapted species often dominate plant communities, suggesting that wildfire is an …

Boreal permafrost soils store large amounts of organic carbon (OC). Parts of this carbon (C)
might be black carbon (BC) generated during vegetation fires. Rising temperature and …

Soil respiration (Rs), the soil‐to‐atmosphere flux of CO2, is a dominant but uncertain part of
the carbon cycle, even after decades of study. This review focuses on progress in …