We assess the role of changing natural (volcanic, aerosol, insolation) and anthropogenic (CO2 emissions, land cover) forcings on the global climate system over the last 150 years using an earth system model of intermediate complexity, CLIMBER-2. We apply several datasets of historical land-use reconstructions: the cropland dataset by Ramankutty & Foley (1999) (R&F), the HYDE land cover dataset of Klein Goldewijk (2001), and the land-use emissions data from Houghton & Hackler (2002). Comparison between the simulated and observed temporal evolution of atmospheric CO2 and delta(13)CO(2) are used to evaluate these datasets. To check model uncertainty, CLIMBER-2 was coupled to the more complex Lund-Potsdam-Jena (LPJ) dynamic global vegetation mo...
Human land-use activities have resulted in large changes to the biogeochemical and biophysical prope...
In this study, vegetation–climate and vegetation–carbon cycle interactions during anthropogenic clim...
ABSTRACT climate with other forcings, climate responses to the changing atmospheric CO2 concentratio...
We assess the role of changing natural (volcanic, aerosol, insolation) and anthropogenic (CO2 emissi...
We assess the role of changing natural (volcanic, aerosol, insolation) and anthropogenic (CO2 emissi...
In older to estimate the effect of historical land cover change (deforestation) on climate, we perfo...
Transient simulations are performed over the entire last millennium with a general circulation model...
The impact of land use on the global carbon cycle and climate is assessed. The Bern carbon cycle-cli...
We explore the ability of the atmospheric CO2 record since 1900 to constrain the source of CO2 from ...
Based on a recent reconstruction of anthropogenic land cover change (ALCC), we derive the associated...
Anthropogenic land cover change (ALCC) is one of the few climate forcings with still unknown sign of...
In order to estimate biogeophysical effects of historical land cover change on climate during last t...
[1] The effects of natural and anthropogenic forcings (solar activity, volcanism, atmospheric CO2 co...
The evidence is now overwhelming that human activity has significantly altered basic element cycles ...
The accumulated biogeophysical impact of historical land use/land cover change (LUCC) on the 20th ce...
Human land-use activities have resulted in large changes to the biogeochemical and biophysical prope...
In this study, vegetation–climate and vegetation–carbon cycle interactions during anthropogenic clim...
ABSTRACT climate with other forcings, climate responses to the changing atmospheric CO2 concentratio...
We assess the role of changing natural (volcanic, aerosol, insolation) and anthropogenic (CO2 emissi...
We assess the role of changing natural (volcanic, aerosol, insolation) and anthropogenic (CO2 emissi...
In older to estimate the effect of historical land cover change (deforestation) on climate, we perfo...
Transient simulations are performed over the entire last millennium with a general circulation model...
The impact of land use on the global carbon cycle and climate is assessed. The Bern carbon cycle-cli...
We explore the ability of the atmospheric CO2 record since 1900 to constrain the source of CO2 from ...
Based on a recent reconstruction of anthropogenic land cover change (ALCC), we derive the associated...
Anthropogenic land cover change (ALCC) is one of the few climate forcings with still unknown sign of...
In order to estimate biogeophysical effects of historical land cover change on climate during last t...
[1] The effects of natural and anthropogenic forcings (solar activity, volcanism, atmospheric CO2 co...
The evidence is now overwhelming that human activity has significantly altered basic element cycles ...
The accumulated biogeophysical impact of historical land use/land cover change (LUCC) on the 20th ce...
Human land-use activities have resulted in large changes to the biogeochemical and biophysical prope...
In this study, vegetation–climate and vegetation–carbon cycle interactions during anthropogenic clim...
ABSTRACT climate with other forcings, climate responses to the changing atmospheric CO2 concentratio...