File tree Expand file tree Collapse file tree
Expand file tree Collapse file tree Original file line number Diff line number Diff line change @@ -101,9 +101,8 @@ step for semi-Lagrangian history transport. It does **not** overwrite
101101` dt_elastic ` — these are independent parameters.
102102
103103A running-average approach for accumulating history when $\Delta t \ll \Delta t_e$
104- was investigated but found to be inaccurate: the BDF constitutive formula
105- inherently couples ` dt_elastic ` to the time between stress evaluations, so
106- the history smoothing cannot compensate for the mismatch. For problems requiring
107- small advection steps with a longer relaxation scale, viscosity clamping
108- (flooring $\eta_ {\text{eff}}$ at the ` dt_elastic ` -derived value) is the
109- recommended approach.
104+ was investigated but found to be extremely diffusive for semi-Lagrangian
105+ transport and is not implemented. To prevent runaway or unstable behaviour
106+ when timesteps become small (e.g. due to CFL constraints or failure events),
107+ we advise limiting the minimum effective viscosity, in line with the physics
108+ of the problem.
You can’t perform that action at this time.
0 commit comments