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Computational Fluid Dynamics (CFD) model was developed for the simulation of the neutrally-stratified atmospheric boundary layer flow over hills, whereas the additional windsource term was implemented into the steady Reynolds-averaged Navier Stokes (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::99966c57c6cf1c77631a305e13ad704e
https://www.bib.irb.hr/1019753
https://www.bib.irb.hr/1019753
