Floodplain Risk Management in Dungog after the April 2015 Super Storm. Presentation Outline

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Presentation Outline Floodplain Risk Management in after the April 2015 Super Storm Rohan Hudson, Royal HaskoningDHV FMA 2017 Preparing for the Next Great Flood 17th May 2017 Background and Flood Mechanisms in The April 2015 Super Storm Model Development and Calibration FRMS - Mitigation Options Assessment Outline of a Suitable Flood Warning System What can we Learn from the Tragedy? Page 2 Flood Mechanisms in (Myall Ck. Catchment Detail) Background is located: in the Upper Hunter Region of New South Wales, approximately 60 km north of Newcastle, and 70 km inland from the coastline. Situated at the confluence of the Williams River and Myall Creek. Population is ~3,000 Page 3 Source Catchment Size Williams River 670 km 2 Myall Creek 74.5 km 2 Town Catchment 1.6 km 2 Common Creek 5.0 km 2 Melbee Estate 0.25 km 2 Page 4 1

Property Inundation in Out of ~1200, properties in, 122 could be flooded above floor level in the PMF In the 1% AEP (100yr ARI) only 22 properties are flooded. In the 5% AEP (20yr ARI) only 9 properties are flooded. Source Catchment Size Number of Properties Williams River 670 km 2 1 property in the 1% AEP (100yr ARI) & 12 properties in PMF (east of railway) Myall Creek (backwater inundation) 74.5 km 2 20 properties in the 100yr ARI & 89 properties in PMF Town Catchment 1.6 km 2 1 property in the 1% AEP (100yr ARI) & 12 properties in PMF. Common Creek 5.0 km 2 no properties in the 1% AEP, 9 properties flooded in April 2015 & PMF Melbee Estate 0.25 km 2 2 properties (d/s of railway embankment) flooded in PMF April 2015 Super Storm The April 2015 Super Storm was driven by a low pressure system on the coast of NSW (i.e. an East Coast Low) The storm produced intense rainfall, high winds & damaging waves Widespread heavy rain occurred from Monday 20th until Wednesday 22nd, with the most intense falls occurring on the morning of Tuesday 21st April Localised super storm cells developed affecting: Stroud,, Cessnock and Maitland In, the storm caused three fatalities, washed 5 houses away and flooded some 80 dwellings (many to ceiling level). Page 5 Page 6 Radar Images Intense rain between 5am and 7am 21/4/2015 Temporal Variation in Rainfall Below graph shows 15 minute rainfall totals for: Post Office (24hr to 9am total is 312mm, 5am to 7am = 175mm) Upper Myall Creek (24hr to 9am total is 190mm, 5am to 7am = 93mm) Source: http://www.theweatherchaser.com/radar-loop/ Page 7 Page 8 Source: (BMT WBM, 2015) 2

Spatial Variation in Rainfall (From Radar Data) Relative Rainfall 4:30 6:30am 21 April 2015 Upper Myall Gauge Less Rain Relative Intensity of April 2015 Comparison of Recorded Rainfall to Design IFD data More Rain Post Office Gauge Note: IFD = intensity frequency duration Source: (BMT WBM, 2015) Source: (BMT WBM, 2015) Page 9 Page 10 Relative Intensity of April 2015 Comparison of Recorded Rainfall to Design IFD data Duration Recorded (mm) Design (ARR87) 100 yr ARI IFD (mm) Design (2016) 100 yr ARI IFD (mm) 1-hour 146 67 77 2-hour 176 93 96 6-hour 241 157 142 9-hour 284 190 168 Myall Creek and Williams River Hydraulic Model 5m grid TUFLOW Model Uses latest LiDAR Elevation Data Complex 2D structures Calibrated to April 2015 Coincident Myall / Williams Extensive sensitivity analysis The recorded 2hr rainfall (176mm) is nearly double the design 100 yr ARI total The design, (critical duration (9hr)), 500yr ARI rainfall is estimated to be 247mm, while the observed, 9hr total was 15% (37mm) higher. Based on design rainfall, the superstorm likely to be in the order of a 1000yr ARI event The 1hr PMP for is 350 mm Page 11 Page 12 3

Limit of Tailwater Influence Williams River Five Properties Destroyed Local Catchment Model Bennett Bridge 2m grid TUFLOW Model Use of Direct Rainfall hydrology 51mAHD 52mAHD Local catchment flooding does not create critical flood levels in the Myall Creek tailwater Rail Bridge 48.5mAHD Long Section 2D model simulating April 2015 event Page 13 Page 14 Comparison of Modelled to Recorded Flood Levels - April 2015 Event Influence of Bennett Bridge Crash Barrier on Flood Levels N O S M T G B A 52.5 Surveyed Peak Flood Level 52 Bridge Obvert / Deck Level 51.5 CD 51 50.5 J 50 49.5 49 Williams River Confluence K 1800 1600 1400 1200 Railway Bridge Bennett Bridge 2000 Myall Creek 2200 Hooke Street Brown Street Mackay Street 2400 1000 X 800 600 Distance Upstream of Williams River Confluence (m) Page 15 400 200 48.5 48 April 2015 Simulated Peak Flood Level (mahd) 53 April 2105 Calibration Event Flood water weiring over crash barrier 47.5 47 0 Page 16 4

Relative Magnitude of April 2015 Flood Comparison of April 2015 Water Levels and Flow to Myall Ck. Design Events AEP / ARI Hooke St Bennett Bridge PeakFlood Level (m AHD) Peak Discharge (m 3 /s) 5% / 20yr 49.41 256 Rate of Rise of April 2015 Flood 2% / 50yr 49.82 324 1% / 100yr 50.2 383 0.5% / 200yr 50.64 444 0.2% / 500yr 51.11 533 PMF (3 x 100yr) 53.00 1174 April 2015 52.00 722 5yr 20yr 100yr 500yr June 2007 49.4 (observed) 250 (est.) April 2015 water level was nearly 1m higher than Myall Ck. 500yr ARI Event April 2015 water level was 1m lower than Myall Ck. PMF Event April 2015 discharge was 1.9 x 100yr ARI discharge Page 17 Page 18 FRMS Mitigation Options Summary Flood modification measures O1) Major Myall Creek (Road and Rail) Bridge Modifications O2) Minor Myall Creek (Road and Rail) Bridge Modifications O3) Myall Creek Levee with Pumps O4) Myall Creek Levee with Diversion Culverts O5) Vegetation Removal with Scour Protection O6) Showground Detention Basin Augmentation O7) North-West Detention Basin Property modification measures O8) Voluntary House Raising (VHR) O9) Voluntary House Purchase (VP) Response modification measures O10) Flood Warning System FRMS Mitigation Options Summary Summary of Peak Flood Levels O1 O2 O4 O5 Design BC O3 Major Minor Levee with Channel Conditions Existing / Levee with Bridge Bridge Diversion Vegetation AEP / ARI Base Case Pumping Upgrade Upgrade Culvert Clearance 20% / 5yr 48.78 48.51 48.57 47.13 48.46 48.56 5% / 20yr 49.41 49.03 49.07 48.31 49.05 49.10 2% / 50yr 49.82 49.31 49.34 48.79 49.23 49.45 1% / 100yr 50.2 49.84 49.89 49.16 49.84 49.99 0.5% / 200yr 50.64 50.25 50.30 49.59 50.05 50.43 0.2% / 500yr 51.11 50.70 50.72 50.12 50.40 50.90 PMF* 53.22 53.18 53.18 53.22 53.22 53.21 April 2015 51.98 50.61 50.82 51.48 51.20 51.61 Page 19 Page 20 5

FRMS Mitigation Options Summary Summary of Damages and B/C Ratios Option Reduction Benefit/Cost NPV of Cost Of Benefit in Option AAD Relative to Damage Option Relative to Damages Base Case Base Case (%) Base Case for Comparison $230k $3.4M n/a n/a n/a n/a O1 - Major Bridge Upgrade $105k $1.56M $6.8M $1.84M 0.27 54% O2 - Minor Bridge Upgrade $126k $1.87M $4.4M $1.53M 0.35 45% O3 - Levee with Pumping (5m3/s) $66k $0.98M $8.0M $2.42M 0.30 71% O4 - Levee with Diversion Culvert $101k $1.5M $7.0M $1.90M 0.27 56% O5 - Channel Vegetation Clearance $138k $2.05M $4.2M $1.35M 0.32 40% 08 - VHR 7 properties, DEMO 6 Properties $159k $2.35M $470,000 $1.04M 2.23 31% FRMS - Flood Warning System Development of a flood warning system for Myall Creek is strongly recommended to reduce risk to life from rapidly rising floodwaters that are capable of inundating a number of low lying properties to above ceiling level in severe events. Given the relatively small number of properties and short evacuation distances, a warning system for the Myall Creek could still be effective in reducing risk to life. Flood Stage vs Property Floor Levels ( Tailwater) Elevation (mahd) 56 55 54 53 52 51 50 49 Floor Level PMF Williams PMF Myall April 2015 500yr ARI 100yr ARI June 2007 5yr ARI 09 - VP 3 properties, VHR 4 properties, DEMO 6 Properties $146k $2.2M $1.2M $1.23M 1.01 36% 48 Jan 2016 47 Page 21 Page 22 0 10 20 30 40 50 60 70 80 90 100 Number of Properties Flooded (above floor level) FRMS - Flood Warning System Recommendations It is recommended that a flood warning system is implemented to reduce fear in the community and protect against further tragedy. A simple rainfall based system, is unlikely to fit in with community expectations of a flood warning system due to the potential for false positive warnings. A water level based flood warning system would provide a higher degree of certainty in the warning and can be more easily related to the degree of flood risk. In order to increase available warning times, the addition of rainfall based triggers is recommended. The use of predicted (i.e. forecast) rainfall products should also be considered, to provide even greater flood warning times. Increased flood warning times would assist emergency services such as the SES coordinate resources during severe flood events. Floodplain Risk Management in after the April 2015 Super Storm Conclusion & Comment April 2015 super storm tragic loss of 3 lives in Royal HaskoningDHV was commissioned to undertake the FRMS&P. Observed flood level: 1.8m above the 1% AEP (100yr ARI). Significantly more properties flooded than ever before. High risk to life may occur when rare events are experienced if near PMF flood level >> 1% AEP flood level. The loss of life of three residents should remind us that a key focus of floodplain risk management activities should be the proactive identification of high risk areas and the implementation of mitigation measures that can prevent future loss of life. It is suggested that State and National Flood Programs include the identification of high risk areas that may occur in rarer events, where risk to life may occur. This could be done by including such a task in their standard briefs for Flood Studies and/or Floodplain Risk Management Studies. A review of existing large catchment studies is also recommended. Page 23 Page 24 6

Thank you Special Thanks to: OEH (Angela Halcrow) Council (Paul Minett) Members of the Floodplain Management Committee And the Community (for input, patience and humour) Page 25 7