Large-scale deforestation and reforestation have contributed substantially to historical and contemporary global climate change in part through albedo-induced radiative forcing, with meaningful implications for forest management aiming to mitigate climate change. Associated warming or cooling varies widely across the globe due to a range of factors including forest type, snow cover, and insolation, but resulting geographic variation remains poorly described and has been largely based on model assessments. This study provides an observation-based approach to quantify local and global radiative forcings from large-scale deforestation and reforestation and further examines mechanisms that result in the spatial heterogeneity of radiative forcin...
We estimated the magnitude of the radiative forcing (RF) due to changes in albedo following the fore...
In the presence of snow, the bias in the prediction of surface albedo by many climate models remains...
We estimated the magnitude of the radiative forcing (RF) due to changes in albedo following the fore...
Large-scale deforestation and reforestation have contributed substantially to historical and contemp...
Large-scale deforestation and reforestation have contributed substantially to historical and contemp...
Widespread anthropogenic land cover change over the last five centuries has influenced the global cl...
Widespread anthropogenic land cover change over the last five centuries has influenced the global cl...
We demonstrate the effectiveness of a new method for quantifying radiative forcing from land use and...
We demonstrate the effectiveness of a new method for quantifying radiative forcing from land use and...
Anthropogenic land cover change (ALCC) influences global mean temperatures via counteracting effects...
A fully coupled land–ocean–atmosphere GCM is used to explore the biogeophysical impact of large-scal...
Forest disturbances are major sources of carbon dioxide to the atmosphere, and therefore impact glob...
Forest disturbances are major sources of carbon dioxide to the atmosphere, and therefore impact glob...
In this study, we assess the climate mitigation potential from afforestation in a mountainous snow-r...
In this study, we assess the climate mitigation potential from afforestation in a mountainous snow-r...
We estimated the magnitude of the radiative forcing (RF) due to changes in albedo following the fore...
In the presence of snow, the bias in the prediction of surface albedo by many climate models remains...
We estimated the magnitude of the radiative forcing (RF) due to changes in albedo following the fore...
Large-scale deforestation and reforestation have contributed substantially to historical and contemp...
Large-scale deforestation and reforestation have contributed substantially to historical and contemp...
Widespread anthropogenic land cover change over the last five centuries has influenced the global cl...
Widespread anthropogenic land cover change over the last five centuries has influenced the global cl...
We demonstrate the effectiveness of a new method for quantifying radiative forcing from land use and...
We demonstrate the effectiveness of a new method for quantifying radiative forcing from land use and...
Anthropogenic land cover change (ALCC) influences global mean temperatures via counteracting effects...
A fully coupled land–ocean–atmosphere GCM is used to explore the biogeophysical impact of large-scal...
Forest disturbances are major sources of carbon dioxide to the atmosphere, and therefore impact glob...
Forest disturbances are major sources of carbon dioxide to the atmosphere, and therefore impact glob...
In this study, we assess the climate mitigation potential from afforestation in a mountainous snow-r...
In this study, we assess the climate mitigation potential from afforestation in a mountainous snow-r...
We estimated the magnitude of the radiative forcing (RF) due to changes in albedo following the fore...
In the presence of snow, the bias in the prediction of surface albedo by many climate models remains...
We estimated the magnitude of the radiative forcing (RF) due to changes in albedo following the fore...