HPC FAQ: Difference between revisions
Content deleted Content added
Line 79:
= With Wu turbulence scheme being the new default, are old models using Smagorinsky wrong? =
Turbulence is pronounced in areas of highly transient flow, e.g. high velocities, bends, ledges and flow contraction/expansion. Where the flow is more benign and/or bed roughness is high, turbulence is not so important as it only applies where there are strong spatial velocity gradients, for example, for uniform flow in a straight rectangular channel the turbulence term is zero as there is no spatial velocity gradient.<br>
The problem with Smagorinsky, which is a large scale eddy turbulence model originally developed for coastal modelling, is that it is cell size dependent (is proportional to cell surface area) and tends to zero as the cell size tends to zero. This has historically not been a major issue as cell sizes have typically been greater than the depth. The general recommendation in the TUFLOW Manual is to be careful of using cell sizes significantly smaller than the depth (see Section 1.4). However, as cells have been becoming finer and finer with the advent of GPU models this issue has increasingly emerged, and is particularly pertinent if using a quadtree or flexible mesh and very small cells relative to the depth are being used. If this is the case, bigger differences will be present for bigger events where the water level and velocities are higher.<br>
TUFLOW, many years ago, changed from purely Constant or purely Smagorinsky to Smagorinsky plus (a small amount of) Constant. This improved absorption of eddies into the streamlines behind a bluff body and helped by varying degrees the modelling at finer cell sizes. This was working well in the time being, however new cell size turbulence scheme has now been implemented to help with the situation even further. <br>
The Smagorinsky/Constant turbulence combination has served the industry well and can continue to be used where the cell sizes are not significantly smaller than the depth where highly transient flows are occurring. If the model is well calibrated (using conventional parameters), continuing to use the Smagorinsky/Constant turbulence option is fine. Therefore, it is not considered that TUFLOW (or other good 2D solvers) have been producing questionable results, but that an improved turbulence representation is needed for 2D schemes with fine-scale cells. This is especially the case for the new Quadtree mesh option and for flexible meshes that utilise fine-scale cells.<br>
With Wu turbulence scheme, the same viscosity parameter(s) can be applied across a wide range of scales from flume tests to large rivers.<br>
| |||