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 name: COSMO-CLM V. 6.0-CLM6
Important reference: Wyard et al. 2017: https://dx.doi.org/10.1002/joc.4879 Resolution: RCM: 12.5km; LAM: 2.8 km
Nr. vertical levels: 40
Time step (s): 80 (12.5 km); 20 (2.8 km)
Important scheme: Two-moment microphysics scheme
Focal time series / severity index: Hail mixing ratio and number concentration, detailed precipitation
Host GCM: ERA-Interim / MPI-ESM
Non-hydrostatic: yes
Van de Vyver, Hans; Van Schaeybroeck, Bert; De Troch, Rozemien; De Cruz, Lesley; Hamdi, Rafiq; Villanueva-Birriel, Cecille; Marbaix, Philippe; van Ypersele, Jean-Pascal; Wouters, Hendrik; Vanden Broucke, Sam; van Lipzig, Nicole P.M.; Doutreloup, Sébastien; Wyard, Coraline; Scholzen, Chloé; Fettweis, Xavier; Caluwaerts, Steven; Termonia, Piet (2021). Regional climate simulations with the UCLouvain COSMO-CLM V. 6.0-CLM6 model. World Data Center for Climate (WDCC) at DKRZ. https://doi.org/10.26050/WDCC/CORDEX.be_UCLouvain_CCLM6-0-6
SQA - Scientific Quality Assurance 'approved by author'
Result Date
2021-04-15
Technical Quality Assurance (TQA)
TQA - Technical Quality Assurance 'approved by WDCC'
Description
1. Number of data sets is correct and > 0: passed; 2. Size of every data set is > 0: passed; 3. The data sets and corresponding metadata are accessible: passed; 4. The data sizes are controlled and correct: passed; 5. The temporal coverage description (metadata) is consistent to the data, time steps are correct: passed; 6. The format is correct: passed; 7. Variable description and data are consistent: passed
Method
WDCC-TQA checklist
Method Description
Checks performed by WDCC. The list of TQA metrics are documented in the 'WDCC User Guide for Data Publication' Chapter 8.1.1
[1] DOIWyard, Coraline; Scholzen, Chloé; Fettweis, Xavier; Van Campenhout, Jean; François, Louis. (2016). Decrease in climatic conditions favouring floods in the south-east of Belgium over 1959-2010 using the regional climate model MAR. doi:10.1002/joc.4879