Hi all,
I recently computed a four domain (25km, 5km, 1km, 200m) simulation and received realistic output. However, after looking through the guidelines I came across the following:
"PBL schemes can be used for most grid sizes when surface fluxes are present; however, at grid size dx << 1 km, this assumption breaks down. To get around this, you can use 3d diffusion instead of a PBL scheme (coupled to surface physics). This works best when dx and dz are comparable."
My simulation was computed with:
bl_pbl_physics = 2, 2, 2, 2,
km_opt = 4, 4, 4, 4,
Yet it appears I should have run it with km_opt = 3 and no pbl scheme for the highest resolution domain.
What kind of impacts might this have had on my simulation? Is it still reasonable?
Thanks,
Ty
I recently computed a four domain (25km, 5km, 1km, 200m) simulation and received realistic output. However, after looking through the guidelines I came across the following:
"PBL schemes can be used for most grid sizes when surface fluxes are present; however, at grid size dx << 1 km, this assumption breaks down. To get around this, you can use 3d diffusion instead of a PBL scheme (coupled to surface physics). This works best when dx and dz are comparable."
My simulation was computed with:
bl_pbl_physics = 2, 2, 2, 2,
km_opt = 4, 4, 4, 4,
Yet it appears I should have run it with km_opt = 3 and no pbl scheme for the highest resolution domain.
What kind of impacts might this have had on my simulation? Is it still reasonable?
Thanks,
Ty