Revision as of 13:13, 8 April 2026 view source Abrar.Alttahir (talk \| contribs) Bureaucrats, Administrators 399 edits →Why are the values of the mapped water level results (h_max) lower than the terrain elevations (DEM_Z)? Tag: Visual edit ← Older edit		Latest revision as of 13:15, 8 April 2026 view source Abrar.Alttahir (talk \| contribs) Bureaucrats, Administrators 399 edits →Why are the values of the mapped water level results (h_max) lower than the terrain elevations (DEM_Z)? Tag: Visual edit
Line 80: == Why are the values of the mapped water level results (h_max) lower than the terrain elevations (DEM_Z)? == As of TUFLOW version 2025.1.1, there is a current limitation affecting result outputs for shallow sheet flow cells on steeper terrain in sub-grid~~-scale~~ sampling (SGS) enabled models. Direct rainfall models are particularly prone to producing substantial areas of shallow sheet flow. In TUFLOW HPC, the cell averaged depth is used computationally and by default in the depth outputs (see below).

TUFLOW Output Discussion: Difference between revisions