Tutorial M10 005 Results QGIS: Difference between revisions

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<li>Open the TUFLOW Viewer.
<li>Open the TUFLOW Viewer.
<li>Select File > Load Results. Navigate to the '''Module_10\TUFLOW\runs''' and open both '''M10_5m_004.tcf''' and '''M10_5m_005.tcf'''.
<li>Select File > Load Results. Navigate to the '''Module_10\TUFLOW\runs''' and open both '''M10_5m_004.tcf''' and '''M10_5m_005.tcf'''.
<li>Select the 'Water Level' map output type in the Result Type panel and toggle on 'Maximum'. Inspect the difference in water levels between M10_5m_004 and M10_5m_005:<br>
<li>Select the 'Water Level' map output type in the Result Type panel and toggle on 'Maximum'. Inspect the difference in water levels between '''M10_5m_004''' and '''M10_5m_005''':<br>
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[[File:Animation M10 005 Results 01.gif]]<br>
[[File:Animation M10 005 Results 01.gif]]<br>

Revision as of 11:58, 27 April 2023

Introduction

QGIS is used to view the water using Non-Newtonian fluids. The results are compared to Newtonian fluids from Part 4. For viewing of the 2D map results, see Module 1.

Method

Inspect water levels of the non-Newtownian outputs:

  1. Open the TUFLOW Viewer.
  2. Select File > Load Results. Navigate to the Module_10\TUFLOW\runs and open both M10_5m_004.tcf and M10_5m_005.tcf.
  3. Select the 'Water Level' map output type in the Result Type panel and toggle on 'Maximum'. Inspect the difference in water levels between M10_5m_004 and M10_5m_005:



  4. Use the Plot Cross Section tool to see the cross section of the water level and bed level at the the edge of the flood extent.
  5. Compare the M10_5m_004 and M10_5m_005 results. The curvature of water level in M10_5m_005 demonstrates the Non-Newtonian fluid qualities. The viscosity of the fluid has changed, becoming more solid, due to the shear force as the fluid moves down the catchment:



Conclusion

  • The water level outputs of the Non-Newtonian fluid were inspected and compared to a Newtonian fluid from Part 4.
  • For further functionality, see TUFLOW Viewer.


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