The LANDMATE Plant Functional Type (PFT) land cover dataset provides gridded, continuous land use and land cover (LULC) information globally tailored to the requirements of regional climate models. The
The LANDMATE PFT dataset provides land cover maps for Europe for the years 1992-2015 in 0.1° (~10km) resolution and a land cover map for Europe for the year 2015 in 0.018° (~2km) resolution. Minor interpolation
The LANDMATE PFT dataset provides a land cover map for Europe for the year 2015 in 0.1° (~10km) and 0.018° (~2km) resolution. The dataset is based on land cover data of the ESA Climate Change Initiative
Evaluation simulations with REMO2020-2-iMOVE performed on the EURO-CORDEX domain at 0.11 degree resolution, using ERA5.1 reanalysis data as lateral boundary conditions for the years 1981-2020, and applying
Earth system model output of LAMACLIMA work package 1 (WP1): idealized global land-use scenarios of cropland expansion, re-/afforestation, irrigation, wood harvest, and reference control
Land use plays a critical role in global mitigation and local adaptation strategies. However, its impacts on local and remote climate and the carbon cycle remain poorly understood across Earth system models
The LUCAS LUC future dataset consists of annual land use and land cover maps from 2016 to 2100 for multiple regions around the globe. It is based on land cover data from the LANDMATE PFT dataset for the
The LUCAS LUC historical dataset consists of annual land use and land cover maps from 1950 to 2015 for multiple regions around the globe. It is based on land cover data from the LANDMATE PFT dataset that
The L1A85 simulation is the model run without landuse change (after yr 2005) and with atmospheric CO2 concentration prescribed from the CMIP run 5.3. This would provide biogeophysical effect of the landuse
The L1B85 simulation is the model run without landuse change (after yr 2005) and with emission-driven atmospheric CO2 concentration from the RCP8.5 scenario. This would provide biogeochemical effect of
The L2A26 simulation is the model run without landuse change (after yr 2005) and with atmospheric CO2 concentration prescribed from the RCP2.6 scenario. This would provide biogeophysical effect of the
The L2A45 simulation is the model run without landuse change (after yr 2005) and with atmospheric CO2 concentration prescribed from the RCP4.5 scenario. This would provide biogeophysical effect of the
The L2A85 simulation is the model run without landuse change (after yr 2005) and with atmospheric CO2 concentration prescribed from the RCP8.5 scenario. This would provide biogeophysical effect of the