Changes between Version 52 and Version 53 of debugging
- Timestamp:
- 07/20/10 11:52:36 (15 years ago)
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debugging
v52 v53 10 10 <tr><th>Surface Slope </th><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td></tr> 11 11 <tr><th>Hutter </th><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#ccc"></td><td bgcolor="#ccc"></td><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#ccc"></td><td bgcolor="#ccc"></td></tr> 12 <tr><th>Hutter/MacAyeal </th><td bgcolor="# fdd"></td><td bgcolor="#fdd"></td><td bgcolor="#ccc"></td><td bgcolor="#ccc"></td><td bgcolor="#fdd"></td><td bgcolor="#fdd"></td><td bgcolor="#ccc"></td><td bgcolor="#ccc"></td></tr>12 <tr><th>Hutter/MacAyeal </th><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#ccc"></td><td bgcolor="#ccc"></td><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#ccc"></td><td bgcolor="#ccc"></td></tr> 13 13 <tr><th>MacAyeal </th><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td><td bgcolor="#dfd"></td></tr> 14 14 <tr><th>Pattyn </th><td bgcolor="#ccc"></td><td bgcolor="#ccc"></td><td bgcolor="#ccc"></td><td bgcolor="#ccc"></td><td bgcolor="#ff9"></td><td bgcolor="#dfd"></td><td bgcolor="#ff9"></td><td bgcolor="#dfd"></td></tr> … … 53 53 - Discontinuous Galerkin: Numerical flux is linked to only one element. If Vx and Vy are discontinuous, we need to create 2 numerical flux: One one the right and one on the left to take into account the discontinuity in velocity 54 54 - in updateVertexPosition each vertices is looking for its new z using their VERTICES DOF in a vector built by the elements using their NODES DOFS 55 - How to create velocity results from discontinuous velocity (Hutter/MacAyeal create a different velocity at the interface) 56 - We should use the depth-averaged velocity of Hutter at the boundary of MacAyeal (in Hutter/MacAyeal models) instead of the velocity on the lower layer