We use a simple statistical approach to reconstruct the global vegetation cover for the LGM (Last Glacial Maximum). Following the IGBP vegetation classification, we divide the land cover into 11 vegetation types plus bare soil. For each of them, we derive a statistical relationship between the probability of its occurrence and climate variables, referred to as the VC-models. The statistical relationships are then CO2 corrected. Using these VC-models without and with CO2 corrections, we reconstructed the vegetation densities under LGM climate conditions based on an ensemble average of 6 GCMs/ESMs of the 3rd Phase of the Paleoclimate Modeling Inter-comparison Project (PMIP3). In deriving the VC-models, the AVHRR vegetation data and the ERA-In...
In current models, the ecophysiological effects of CO₂ create both woody thickening and terrestrial ...
Reconstruction of climate anomalies for the Last Glacial Maximum (LGM, ca 21,000 years ago), made by...
International audienceVegetation reconstructions from pollen data for the Last Glacial Maximum (LGM)...
We use a simple statistical approach to reconstruct the global vegetation cover for the LGM (Last Gl...
We provide an estimate of global vegetation density for the Last Glacial Maximum (LGM) using a simpl...
We present a new global reconstruction of seasonal climates at the Last Glacial Maximum (LGM, 21 000...
The global vegetation response to climate and atmospheric CO₂ changes between the last glacial maxim...
The global vegetation response to climate and atmospheric CO2 changes between the last glacial maxim...
The global vegetation response to climate and atmospheric CO2 changes between the last glacial maxim...
A simplified three‐dimensional global climate model was used to simulate the surface temperature and...
Vegetation is an important component in the Earth system, providing a direct link between the biosph...
A simplified three-dimensional global climate model was used to simulate the surface temperature and...
Abstract. Vegetation reconstructions from pollen data for the Last Glacial Maximum (LGM), 21 ky ago,...
In current models, the ecophysiological effects of CO₂ create both woody thickening and terrestrial ...
Reconstruction of climate anomalies for the Last Glacial Maximum (LGM, ca 21,000 years ago), made by...
International audienceVegetation reconstructions from pollen data for the Last Glacial Maximum (LGM)...
We use a simple statistical approach to reconstruct the global vegetation cover for the LGM (Last Gl...
We provide an estimate of global vegetation density for the Last Glacial Maximum (LGM) using a simpl...
We present a new global reconstruction of seasonal climates at the Last Glacial Maximum (LGM, 21 000...
The global vegetation response to climate and atmospheric CO₂ changes between the last glacial maxim...
The global vegetation response to climate and atmospheric CO2 changes between the last glacial maxim...
The global vegetation response to climate and atmospheric CO2 changes between the last glacial maxim...
A simplified three‐dimensional global climate model was used to simulate the surface temperature and...
Vegetation is an important component in the Earth system, providing a direct link between the biosph...
A simplified three-dimensional global climate model was used to simulate the surface temperature and...
Abstract. Vegetation reconstructions from pollen data for the Last Glacial Maximum (LGM), 21 ky ago,...
In current models, the ecophysiological effects of CO₂ create both woody thickening and terrestrial ...
Reconstruction of climate anomalies for the Last Glacial Maximum (LGM, ca 21,000 years ago), made by...
International audienceVegetation reconstructions from pollen data for the Last Glacial Maximum (LGM)...