Measurements of micrometeorological variables were made for two snow-free periods at a Restored vacuum harvested and non-restored (Comparison) section of a peatland in eastern Québec, Canada. Measurements of evapotranspiration and surface heat fluxes were obtained using an eddy correlation energy balance system at the Restored site and a combination Priestley– Taylor and lysimeter approach at the Comparison site. At the ecosystem scale, the energy, water and gas exchange processes are strongly coupled. Through harvesting, a peatland may lose most of its surface vegetation cover, altering the thermal regime of the peat, while the drier conditions required for the harvesting drastically alters the system’s hydrology. The measurements indicat...
In this study latent heat flux (λE) measurements made at 65 boreal and arctic eddy-covariance (EC) s...
SummaryBoreal peatland energy balances using the eddy covariance technique have previously been made...
Observations of heat and moisture exchange were made over saturated Sphagnum moss in a grass-covered...
Surface–atmosphere energy exchange is strongly ecosystem-specific. At the same time, as the energy b...
An understanding of the symbiotic water and gas exchange processes at the ecosystem scale is essenti...
The natural carbon storage function of peatland ecosystems can be severely affected by the abandonme...
Hydrological conditions play a key role in the carbon cycle of northern peatlands. This study examin...
Boreal peatland energy balances using the eddy covariance technique have previously been made in Ala...
Peatlands and forests cover large areas of the boreal biome and are critical for global climate regu...
Continuous measurements of ecosystem scale evapotranspiration (ET) were obtained using the eddy cova...
Water and energy fluxes from a treed peat plateau in a wetland-dominated discontinuous permafrost ba...
Mires surface energy and water budgets govern the conditions for climatic, hydrological, ecological ...
This study examined (i) the effect of artificially created microtopography and straw mulch on the so...
Typical bogs in the boreal forest zone can be characterised by hummock and hollow micro-topography a...
Peatland ecosystems store between 200 and 450 Gt C (1015 gC). It is estimated that peatlands constit...
In this study latent heat flux (λE) measurements made at 65 boreal and arctic eddy-covariance (EC) s...
SummaryBoreal peatland energy balances using the eddy covariance technique have previously been made...
Observations of heat and moisture exchange were made over saturated Sphagnum moss in a grass-covered...
Surface–atmosphere energy exchange is strongly ecosystem-specific. At the same time, as the energy b...
An understanding of the symbiotic water and gas exchange processes at the ecosystem scale is essenti...
The natural carbon storage function of peatland ecosystems can be severely affected by the abandonme...
Hydrological conditions play a key role in the carbon cycle of northern peatlands. This study examin...
Boreal peatland energy balances using the eddy covariance technique have previously been made in Ala...
Peatlands and forests cover large areas of the boreal biome and are critical for global climate regu...
Continuous measurements of ecosystem scale evapotranspiration (ET) were obtained using the eddy cova...
Water and energy fluxes from a treed peat plateau in a wetland-dominated discontinuous permafrost ba...
Mires surface energy and water budgets govern the conditions for climatic, hydrological, ecological ...
This study examined (i) the effect of artificially created microtopography and straw mulch on the so...
Typical bogs in the boreal forest zone can be characterised by hummock and hollow micro-topography a...
Peatland ecosystems store between 200 and 450 Gt C (1015 gC). It is estimated that peatlands constit...
In this study latent heat flux (λE) measurements made at 65 boreal and arctic eddy-covariance (EC) s...
SummaryBoreal peatland energy balances using the eddy covariance technique have previously been made...
Observations of heat and moisture exchange were made over saturated Sphagnum moss in a grass-covered...