Discuss advection schemes, timestepping, pressure gradients, coordinates, etc.
I've been looking through the WRF code to find how the lower boundary conditions are set. So far I've found the vertical wind lower boundary condition through the subroutine set_w_surface inside /dyn_em/module_bc_em.F. However, I am still unable to find what the lower boundary conditions for u and v are. I am running an idealized tropical cyclone case using sfclay surface scheme and YSU PBL scheme. Any help with this will be greatly appreciated.
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