Soil hydrological processes (SHP) support ecosystems, modulate the impact of climate
change on terrestrial systems and control feedback mechanisms between water, energy and …

The global forest carbon (C) stock is estimated at 662 Gt of which 45% is in soil organic
matter. Thus, comprehensive understanding of the effects of forest management practices on …

The response of evapotranspiration (ET) to warming is of critical importance to the water and
carbon cycle of the boreal biome, a mosaic of land cover types dominated by forests and …

Fire behaviour is changing in many regions worldwide. However, nonlinear interactions
between fire weather, fuel, land use, management and ignitions have impeded formal …

Abstract Purpose of Review The Arctic has experienced the most rapid change in climate of
anywhere on Earth, and these changes are certain to drive changes in the carbon budget of …

Climate change threatens the capacity of peatlands to continue storing carbon (C)
belowground. Microorganisms are crucial in regulating the peatland C sink function, but how …

When a peatland is drained and cultivated, it behaves as a notable source of CO2. However,
we lack temporally and spatially explicit estimates of carbon losses from cultivated …

Aim Persistent sinks of atmospheric CO2 in undisturbed peatlands are not included in future
projections of the global carbon budget. We aimed to explore possible responses of …

Despite peatlands' important feedbacks on the climate and global biogeochemical cycles,
predicting their dynamics involves many uncertainties and an overwhelming variety of …

Earth system models (ESMs) are our primary tool for projecting future climate change, but
their ability to represent small-scale land surface processes is currently limited. This is …