TUFLOW Output Discussion: Difference between revisions

Content deleted Content added

Revision as of 09:49, 2 March 2026 view source Anne.Kolega (talk \| contribs) Bureaucrats, Administrators 184 edits m →How to create a maximum grid for datasets without direct maximum output from a TUFLOW run?: deleted a comma ← Older edit		Latest revision as of 13:15, 8 April 2026 view source Abrar.Alttahir (talk \| contribs) Bureaucrats, Administrators 397 edits →Why are the values of the mapped water level results (h_max) lower than the terrain elevations (DEM_Z)? Tag: Visual edit
(One intermediate revision by the same user not shown)
Line 80: == Why are the values of the mapped water level results (h_max) lower than the terrain elevations (DEM_Z)? == As atof TUFLOW ~~Build~~version 252025.1.1, there is a current limitation ~~for~~affecting result outputs atfor shallow sheet flow cells on steeper terrain in sub-grid~~-scale~~ sampling (SGS) enabled models. Direct rainfall models are particularly prone to ~~result in~~producing substantial ~~extents~~areas of shallow sheet flow. In TUFLOW HPC, the cell averaged depth is used computationally and by default in the depth outputs (see below).