Revision as of 11:49, 3 September 2025 view source Pavlina Monhartova (talk \| contribs) Bureaucrats, Administrators 5,365 edits →Groundwater Linking to 1D (ESTRY or SWMM) ← Older edit		Latest revision as of 17:31, 3 September 2025 view source Pavlina Monhartova (talk \| contribs) Bureaucrats, Administrators 5,365 edits →Why does the groundwater lateral flux calculation include porosity, and what changes are planned?
Line 132: Fine-tuning soil properties, hydraulic conductivity, and boundary conditions will improve interflow simulation accuracy. == Why does the groundwater lateral flux calculation include porosity~~, and what changes are planned~~? == Benchmarking tests have identified that the current sub surface flow equation in TUFLOW underestimates steady state discharge rates due to the inclusion of porosity. While the steady state water level gradient is correct, transient state simulations show discrepancies.

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