Peatlands and forests cover large areas of the boreal biome and are critical for global climate regulation. They also regulate regional climate through heat and water vapour exchange with the atmosphere. Understanding how land-atmosphere interactions in peatlands differ from forests may therefore be crucial for modelling boreal climate system dynamics and for assessing climate benefits of peatland conservation and restoration. To assess the biophysical impacts of peatlands and forests on peak growing season air temperature and humidity, we analysed surface energy fluxes and albedo from 35 peatlands and 37 evergreen needleleaf forests - the dominant boreal forest type - and simulated air temperature and vapour pressure deficit (VPD) over hyp...
Surface–atmosphere energy exchange is strongly ecosystem-specific. At the same time, as the energy b...
We estimated the magnitude of the radiative forcing (RF) due to changes in albedo following the fore...
We assessed the vulnerability of blanket peat to climate change in Great Britain using an ensemble o...
Peatlands and forests cover large areas of the boreal biome and are critical for global climate regu...
Peatlands and forests cover large areas of the boreal biome and are critical for global climate regu...
The response of evapotranspiration (ET) to warming is of critical importance to the water and carbon...
Boreal peatlands are important ecosystems from a carbon balance perspective because they are natural...
Boreal peatlands are important ecosystems from a carbon balance perspective because they are natural...
[1] Forested peatlands represent an important global carbon pool, storing 48.0 Pg of carbon within c...
Surface-atmosphere energy exchange is strongly ecosystem-specific. At the same time, as the energy b...
Surface-atmosphere energy exchange is strongly ecosystem-specific. At the same time, as the energy b...
Land use, land use change, and forestry (LULUCF) have been directly altering climate, and it has bee...
The majority of the world’s peatlands are located in northern regions where climate change is occurr...
Peatland ecosystems store between 200 and 450 Gt C (1015 gC). It is estimated that peatlands constit...
In a climate model, surface energy and water fluxes of the vegetated ecosystem largely depend on imp...
Surface–atmosphere energy exchange is strongly ecosystem-specific. At the same time, as the energy b...
We estimated the magnitude of the radiative forcing (RF) due to changes in albedo following the fore...
We assessed the vulnerability of blanket peat to climate change in Great Britain using an ensemble o...
Peatlands and forests cover large areas of the boreal biome and are critical for global climate regu...
Peatlands and forests cover large areas of the boreal biome and are critical for global climate regu...
The response of evapotranspiration (ET) to warming is of critical importance to the water and carbon...
Boreal peatlands are important ecosystems from a carbon balance perspective because they are natural...
Boreal peatlands are important ecosystems from a carbon balance perspective because they are natural...
[1] Forested peatlands represent an important global carbon pool, storing 48.0 Pg of carbon within c...
Surface-atmosphere energy exchange is strongly ecosystem-specific. At the same time, as the energy b...
Surface-atmosphere energy exchange is strongly ecosystem-specific. At the same time, as the energy b...
Land use, land use change, and forestry (LULUCF) have been directly altering climate, and it has bee...
The majority of the world’s peatlands are located in northern regions where climate change is occurr...
Peatland ecosystems store between 200 and 450 Gt C (1015 gC). It is estimated that peatlands constit...
In a climate model, surface energy and water fluxes of the vegetated ecosystem largely depend on imp...
Surface–atmosphere energy exchange is strongly ecosystem-specific. At the same time, as the energy b...
We estimated the magnitude of the radiative forcing (RF) due to changes in albedo following the fore...
We assessed the vulnerability of blanket peat to climate change in Great Britain using an ensemble o...