prabhakar_1510
New member
Hi!
Do the surface turbulent fluxes (sensible and latent heat) simulated from the WRF model only depend on the computations performed in the surface layer scheme (e.g., revised MM5 surface layer scheme)? Or does the land surface model (e.g., Noah-MP LSM) also affect the final output for these two variables?
If so, please explain briefly how the two schemes interact with each other.
Thanks
Do the surface turbulent fluxes (sensible and latent heat) simulated from the WRF model only depend on the computations performed in the surface layer scheme (e.g., revised MM5 surface layer scheme)? Or does the land surface model (e.g., Noah-MP LSM) also affect the final output for these two variables?
If so, please explain briefly how the two schemes interact with each other.
Thanks