This post has materials that explain why the MRGO did not increase the flooding of New Orleans during Hurricane Katrina.
Article – The Hurricane Katrina Levee Breach Litigation: Getting the First Geoengineering Liability Case Right. (alternative source)
The MRGO channel does not contribute significantly to peak surge during severe storms, when the conveyance of surge is dominated by flow across the entire surface of the coastal lakes and marsh. Nor does the channel contribute significantly to wave run-up. p. ES-2
Attachment: Numerical Modeling of Storm Surge Effect of MRGO Closure
Figure 1 | Project Area |
Figure 2 | Corps Estimate of Regional Inundation from Category 4 and Above Storm Surge |
Figure 3 | LWRRI Estimate of Regional Inundation from Hurricane Georges (1998) Prior to Track Turn |
Figure 4 | Full 2003 ACIRC Grid |
Figure 5 | Detail of 2003 ADCIRC Grid for MRGO and Surrounding Area |
Figure 6 | 3D Depiction of 2003 ADCIRC Terrain for MRGO and Surrounding Area |
Figure 7 | Comparison of Surveyed versus 2003 ADCIRC MRGO Channel Near Shell Beach, Plan |
Figure 8 | Comparison of Surveyed versus 2003 ADCIRC MRGO Channel Near Shell Beach, Cross Section |
Figure 9 | Tracks for Hurricane Simulations |
Figure 10 | 3D Depiction of 2003 ADCIRC Terrain with Closed MRGO |
Figure 11 | Maximum WSE for 124-Knot-Fast Storm, Baseline MRGO |
Figure 12 | Maximum WSE for 124-Knot-Fast Storm, Closed MRGO |
Figure 13 | Difference in Maximum WSE for 124-Knot-Fast Storm, Baseline versus Closed MRGO |
Figure 14 | Storm Surge Stage Hydrographs, 124-Knot-Fast Storm, Baseline versus Closed MRGO |
Figure 15 | Maximum WSE for Hurricane Betsy, Baseline MRGO |
Figure 16 | Maximum WSE for Hurricane Betsy, Closed MRGO |
Figure 17 | Difference in Maximum WSE for Hurricane Betsy, Baseline versus Closed MRGO |
Figure 18 | Storm Surge Stage Hydrographs, Hurricane Betsy, Baseline versus Closed MRGO |
Figure 19 | Storm Surge Current Speed Hydrographs, Hurricane Betsy, Baseline versus Closed MRGO |
Figure 20 | Hurricane Katrina Simulation |
Figure 21 | Maximum WSE for Hurricane Katrina, Baseline MRGO |
Figure 22 | Maximum WSE for Hurricane Katrina, Closed MRGO |
Figure 23 | Difference in Maximum WSE for Hurricane Katrina, Baseline versus Closed MRGO |
Figure 24 | Storm Surge Hydrographs, Hurricane Katrina, Baseline versus Closed MRGO |
Figure 25 | Storm Surge Current Speed Hydrographs, Hurricane Katrina, Baseline versus Closed MRGO |
Figure 26 | Baseline 2003 ADCIRC Levees |
Figure 27 | Modified Levees |
Figure 28 | Maximum WSE for Hurricane Katrina, Modified Levees and Closed MRGO |
Figure 29 | Difference in Maximum WSE for Hurricane Katrina, Baseline versus Modified Levees |
Figure 30 | Storm Surge Hydrographs, Hurricane Katrina, Baseline versus Modified Levees |
Figure 31 | Schematic of Wave Set-up and Run-up |
Figure 32 | HPL Cross Section near Bayou Dupre, Station 673 |
Figure 33 | Lake Borgne to HPL Levee @ Bayou Dupre Transect for Wave Run-up Analysis |
Figure 34 | Schematic of Wave Generation and Attenuation for Lake Borgne to HPL Levee @ Bayou Dupree |
Figure 35 | 3D Depiction of Higher Resolution ADCIRC Terrain for MRGO and Surrounding Area with Closed MRGO |