INLAND DVGM output - SSP1-RCP2.6 and SSP3-RCP8.5

We used the INLAND DGVM model to simulate the water and carbon cycle in the present climate and also under two different CC and LUC scenarios. To stabilize the carbon and water stocks, we used a 500-years spin up run, with dynamic vegetation, performed with historical data from CRU-JRA (Climatic Research Unit and Japanese reanalysis - detailed by Harris, 2019). After that, we started the two different scenario and recorded the model outputs from 2016 to 2095 (80 years), in a 0.5 X 0.5 degrees grid (latitude AND longitude).

The meteorological forcing and CO2 concentration are taken from HADGEM2-ES (Collins et al., 2011),  from ISIMIP[1] Project (Inter-Sectorial Impact Model Intercomparison Project), from 2b Repository (https://data.isimip.org/), described at Frieler et al., 2017. We choose to use the Bias corrected data. As input of land use and land cover maps, we used the refined regional scenarios provided by (Bezerra et al., 2022), data available at https://zenodo.org/record/5123560#.YVJFzzlv80M (Bezerra et al., 2021),

[1] https://www.isimip.org/documents/564/ISIMIP2b_protocol_210131_noEnergy_IV_JS-1_IV_pmp-1.pdf