Hello everyone,I am preparing a high-resolution WRF simulation over a complex mountainous region in the Italian Alps. My planned nested domains have horizontal grid spacings of approximately:
- d01: 9 km
- d02: 3 km
- d03: 1 km
- d04: 333 m
My main questions are:
- For WRF terrain elevation and HGT_M, is a bare-earth DTM generally more physically appropriate than a DSM?
- Could using a DSM introduce an artificial elevation bias in forested or urban areas?
- For a 333 m inner domain over steep Alpine terrain, what source resolution would be appropriate before interpolation to the WRF grid—for example 10 m, 30 m, or 100 m?
- Should a very high-resolution LiDAR DTM be averaged or smoothed before converting it into WPS geogrid format?
- Are there recommended smoothing criteria or terrain-slope checks to avoid numerical instability at 333 m grid spacing?
- Is it advisable to use the same terrain dataset for all nested domains, or can a local LiDAR DTM be used only for the innermost domain while a global DEM is used for the outer domains?
- If local DTM and global DEM datasets are combined, what is the recommended method for blending them near the dataset boundaries?
I would appreciate any recommendations regarding suitable datasets, preprocessing steps, WPS configuration, and relevant references or previous experience.
Thank you.