FMA Challenge 3: Difference between revisions
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==Boundary Conditions==
The 1d/2d linking was along the top of the levee. The elevations along these levees were extracted from the 10ft DEM, these and other significant features were included in the TUFLOW model as 3D GIS breakline layers, ensuring the hydraulic control is represented in the grid regardless of cell size.▼
===Open Boundaries===
All outflow from the model was assumed to be only via the main channel (ie. there was no water level boundary applied to the 2D overbank domain).
===1D/2D Linking===
▲The
==Non-Infiltration Results==
The flood extent from the 100ft 2D grid model is shown below.
[[File:FMA3_3.jpg|600px]]
As discussed in the Manning’s n table above, the main creek n value of 0.20 is considered very high, especially in the lower reaches of the study area. A sensitivity analysis was carried out by lowering all the Manning’s n values in the main channel (modeled as 1D cross-sections) to 0.10.
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