Hello everyone,
I am currently working with the WRF-Hydro model, and I am using the Muskingum-Cunge method for channel routing. I have a question regarding the hydrological processes when the User-Defined Mapping (UDMP) option is enabled versus disabled.Aside from the differences in sub-basin delineation and river network structure, I would like to know whether there are any differences in the physical processes of routing between these two configurations.
Thank you very much for your time and assistance.
Best regards,
Zed Li