The experiment aims to investigate how the representation of convection influences the West African Monsoon during the mid-Holocene.
Atmospheric and SST input data originate from the MPI-ESM Holocene
The experiment aims to investigate how the representation of convection influences the West African Monsoon during the mid-Holocene.
Atmospheric and SST input data originate from the MPI-ESM Holocene
Regional climate simulations with the MAR V 3.9 model by University of Liège.
Dynamical downscaling on the CORDEX EUR-11 domain and HRes domain over Belgium at convection-permitting scale.
Model
Regional climate simulations with the COSMO-CLM V. 6.0-CLM6 model by UCLouvain.
Dynamical downscaling on the CORDEX EUR-11 domain and HRes domain over Belgium at convection-permitting scale.
Model
Regional climate simulations with the ALARO-0 model by the Royal Meteorological Institute of Belgium and Ghent University (RMIB-UGent).
Dynamical downscaling on the CORDEX EUR-11 domain and HRes domain
Present climate data (1991-2022) at very-high spatial resolution (1 km) for Sierra Nevada, the highest mountain region in the Iberian Peninsula located in southeastern Andalusia (Spain). Data obtained
Pseudo-projected climate data (1991-2020 + climate change signal of a set of 24 CMIP6 GCMs for the period 2070-2099 under the SSP5-8.5) at very-high spatial resolution (1 km) for Sierra Nevada, the highest
The objective of the project is to better understand what controls the size of intense storms, also known as deep convective systems. The larger the storm is the more it has consequences in terms of extreme