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HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 1SEPTEMBER 2010
FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
William VeerbeekFLOOD RESILIENCE GROUP | WE Department | Unesco-IHEWestvest 7 | P.O. Box 3015 | 2601DA Delft | NetherlandsT: +31(0)15 2151 821 | M: +31(0)6 427 88 359w.veerbeek@fl oodresiliencegroup.orgwww.fl oodresiliencegroup.org
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 2
Assess potential fl ood hazard and impact for the unembanked areas in the • Rijnmond-Drechtsteden region;Include climate change scenarios;• Apply a high level of detail;• Include regional adaptation option: Closable but Open.•
RESEARCH OBJECTIVES
Flood impact Urban area
Flood extent & depth
Flow velocitiesFlood impact
Port area
Climate Change scenarios
Closable Open Rijnmond
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 3
Located along the Meuse & Merwede (Waal) rivers;• 30,000 housing units, 64,000 inhabitants;• Port of Rotterdam;• High level of diff erentiation (physical, functional, historical, etc.);• Unembanked area, often high level of elevation (sedimentation & man-made).•
RIJNMOND-DRECHTSTEDEN: CHARACTERISTICS
Veerbeek et al, 2010
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 4
1. FLOOD HAZARD
FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 5
Inundation depths derived from 1D-Hydraulic model HSRR03b • (Stijnen & Slootjes, 2010), for current, G+ 2050 and Veerman 2100 scenarios & Closable but Open;5x5m DEM resolution;• GIS extrapolation of observed water stages;• Flood velocities through existing hydraulic models and measurements;• Failure rate of Maeslant & Hartel storm surge barrier;• Range of return periods: 10, 50, 100, 1000, 2000, 4000, 10000 years.•
FLOOD MODEL: METHODOLOGY
Climate Change Rhine Discharge Meuse Discharge Sea level rise [m] Storm duration [h] Scenario at Lobith [m3/s] at Borgharen [m3/s]
Current Conditions (2010) 16,000 3,800 0 29KNMI’06 G+ (2050) 18,000 4,600 0.60 35VEERMAN (2100) 18,000 4,600 1.30 35
Lansen et al, 2010DEM of the Rijnmond-Drechtsteden area
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 6
10Return Period
10002000400010000
100
Many natural fl oodplains are fl ooded for low return periods (e.g. 10y)• Urban areas are generally fl ooded only during ‘extreme events’• Newer port areas (Rotterdam & Dordrecht) are relatively ‘safe’•
OBSERVED FLOOD EXTENT (CURRENT CONDITIONS)
Based on Huizinga et al, 2010
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 7
Within urban areas observed fl ood extent diff ers signifi cantly• Treshold eff ects and gradual fl ooding•
OBSERVED FLOOD EXTENT (CURRENT CONDITIONS)
10Return Period
10002000400010000
100
Noordereiland/Piekstraat Rotterdam• Inundation for low return periods• Main streets fl ooded during ‘extreme • events’
Based on Huizinga et al, 2010
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 8
8000
9000
10000
11000
12000
13000
14000
15000
16000
17000
0 2000 4000 6000 8000 10000 12000
Return period (years)
Floo
ded
area
(ha)
2010205021002050_lockable/open2100_lockable/open
Flood extent for the range of return periods
Climate change scenarios increase fl ood extent signifi cantly;• Closable but Open option does not lead to reduction;• Failure rate Maeslant/Hartel storm surge barier is critical.•
OBSERVED FLOOD EXTENT
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 9
200Depth [cm]
0
Signifi cant variations in inundation depths also outside natural fl oodplains;• For medium return periods (e.g. 100y): Generally low inundation depths in highly • populated areas;Some exceptions (e.g. Noordereiland/Piekstraat area)•
OBSERVED INUNDATION DEPTHS
Noordereiland/Piekstraat Rotterdam• EP = 1/100, Current conditions• Signifi cant fl ood depths observable • within residential areas
Based on Huizinga et al, 2010
Locally more than 1m of inundation
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 10
MAASSLUISSTADSHAVENS
VAN BRIENENOORDBRUG
STADSWERVEN
High fl ow velocities only at the Western end of the river mouth (North-Sea);• Flow velocities on quays expected to range between 0.1 and 0.25 m/s;• Further inland even lower (high hydraulic roughness due to built-up areas);• Climate change scenarios will not increase velocities signifi cantly;• Conclusion: Low probability of structural damages and casualties/injuries. •
FLOW VELOCITIES
Asselmans, 2010
Calculated fl ow velocities main channel: low fl ow conditions combined with a severe storm surge
-2.5
-2
-1.5
-1
-0.5
0
0.5
1
1.5
2
12:00 00:00 12:00 00:00 12:00 00:00
time (hours)
flow
vel
ocity
(m/s
)
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 11
2. FLOOD IMPACT
FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 12
Estimate DIRECT fl ood damages;• High level of detail: individual housing units, infrastructure and public space;• Derive damage composition;• Perform analysis on spatiotemporal distribution of damages;•
Refi nement from existing fl ood damage model used in UFM-Dordrecht • (Veerbeek et al, 2009);Introduction of specifi c housing characteristics through Google Streetview;• Adapt model to 5x5m cells;• Model is synthetic; damage curves developed icw building/insurance sector.•
(URBAN) FLOOD DAMAGE MODEL: METHODOLOGY
Kennis voor Klimaat Knowledg
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 13
Hardly any noticeable threshold eff ects;• Small trend change for G+ 2050 and Veerman 2100 at 1000-year return period;• EAD: Increase for G+ (2050) 75%, Veerman (2100) 147%• 100 fold increase: Current 1000-year level becomes 10-year level (Veerman 2100)•
0
25
50
75
100
125
150
175
10 100 1000 10000
return period [Y]
exp
ect
ed
Dam
ag
e [
m€
]
Current 2050 G+
2100 Veerman 2050 Closable but open
2100 Closable but open
(URBAN) FLOOD DAMAGE MODEL: AGGREGATE DAMAGES
y = 4E-08x5.8845
0
20
40
60
80
100
120
140
160
180
225 250 275 300 325 350 375 400 425 450
water stage [cm +NAP]
exp
ect
ed
Dam
ag
e [
m€
]
Expected aggregate fl ood damages for RPs
Expected aggregate fl ood damages for water stages
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 14
Cleaning & drying, 11%
Floor & w all, 11%
Doors & w indow4%
Kitchen, 8%
Installations, 19%
Contents Damage, 48%
Infrastructure/public space: currently 20% of EAD;• Climate change scenarios hardly change this ratio .• Housing: Damage to furnishing about 50%.•
0
10
20
30
40
50
60
10 50 100 1000 2000 4000 10000
return period [Y]
expec
ted D
amag
e [m
€]
Cleaning & drying Floor & wall Doors & windows
Kitchen Installations Contents Damage
Damage compostion (housing) for the Veerman 2100 scenario
(URBAN) FLOOD DAMAGE MODEL: DAMAGE COMPOSITION
What fl ood damage reduction level can be achieved with an ef-fective early warning strategy?
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 15
-500
500
1500
2500
-1900 1900-1920 1920-1940 1940-1960 1960-1980 1980-2000 2000+Construction period
# flo
oded
housi
ng u
nits
10 50 100
-500
500
1500
2500
-1900 1900-1920 1920-1940 1940-1960 1960-1980 1980-2000 2000+Construction period
# f
looded
housi
ng u
nits
10 50 100
0
1000
2000
3000
-1900 1900-1920 1920-1940 1940-1960 1960-1980 1980-2000 2000+
Construction period
# f
looded
housi
ng u
nits
10 50 100
Current Conditions
G+ Scenario 2050
Veerman Scenario 2100
Distribution of fl ooded buildings over the age of the building stock (10, 50, 100y);• Dramatic increase of fl ooded monumental buildings (e.g. Dordrecht)•
(URBAN) FLOOD DAMAGE MODEL: AGE BUILDING STOCK
Damage distribtuion over the age of the building stock
Is increasing fl ood risk a threat to our cultural heritage?
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 16
(URBAN) FLOOD DAMAGE MODEL: ABSOLUTE VS RELATIVE DMGS
Relative dmgs: expected dmg over the total building stock per municipality;• Substantial diff erences between municipalities: rate, behavior; absolute, relative;• Infl uence of climate change scenarios changes distribution;• Avg. EAD Rotterdam: € 4 (current) to € 29 (2100 Veerman);• Avg. EAD Bergambacht: € 614 (current) to € 660 (2100 Veerman).•
RotterdamDordrechtNederlekBergambacht0
5
10
15
20
25
30
35
40
45
50
55
60
65
70
75
10 100 1000 10000
return period [mY]
exp
ect
ed
Dam
ag
e [
m€
]
Bergambacht Dordrecht Nederlek Rotterdam
0
5
10
15
20
25
30
35
40
45
10 50 100 1000 2000 4000 10000
return period [mY]
exp
ect
ed
Dam
ag
e [
k€
]
Rotterdam Dordrecht Nederlek Bergambacht
Expected damages for the Veerman 2100 scenario: absolute (left) and relative (right) Do these fi gures indicate possible responses (structural / non-struc-tural)?
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 17
(URBAN) FLOOD DAMAGE MODEL: DAMAGE HOTSPOTS
50% fl ood damages located in 15% of the damage clusters: highly concentrated;• Importance of individual clusters changes for higher return periods (threshold ef-• fects)
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 18
(PORT) FLOOD DAMAGE ASSESSMENT: METHODOLOGY
No ‘standard’ application of stage-damage curves possible;• Existing risk assessment framework is extremely complex;• Potentially high level of indirect tangible and intangible damages;•
Focus on:• Infrastructure, utility-lifeline (electricity, gas, etc.);• Assessment of additional fl ood risk i.r.t. existing risk profi le for chemical plants. •
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 19
Effect of flooding Probability of damage given a flooding event
Casualties Societal disruption
Environment Economical damage
Berthing facilities Washout due to water run-off Quay wall CorrosionJetties Failure of berthing functionTerminal Roads and terrain not accessibleTerrain Washout due to water run-off Roads and railwaysUnderground facilities Rupture of pipe linesElectricity Failure and damage of electricity and ICT
Communication Failure and damage of communication Cables Pipe linesGeneral facilities Washing away of loose standing objects
Lighting buildings Lighting failure Safety installations Safety onsite cannot be guaranteedVehicles Damage to buildings
Effect of flooding Probability of damage given a flooding event
Casualties Societal disruption
Environment Economical damage
Facilities Cable trays are on ground level => spills + release of toxic goods + interruption of processes. Instability of construction of installation, for instance distillation columns built on footings
Process installations Rupture / damage of (empty) pipelines Pipelines Corrosion of (salt) water in installations Cooling installation Power failure => uncontrollable processes
Storage of goods Rupture of (oil) tanks due to high water pressures
Oil LNG cooled storaged=> during power failure uncontrolled boil-off
LNG (Controlled) shut-down installations during flood threat
LPG Release toxic material from storage Toxic gasses: H2F Gas supply fo electricity / hinterland
interrupted Vegetable oil
Qualitative assessment of vulnerability: Liquid bulk
Qualitative assessment of vulnerability: General harbour facilities
(PORT) FLOOD DAMAGE ASSESSMENT: EXPERT SESSION
Expert judgment to develop a qualitative assessment of fl ood impact•
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 20
(PORT) FLOOD DAMAGE ASSESSMENT: CHEMICAL INSTALLATIONS
Main question: What is the additional risk of 1m of inundation?• BowTie model to assess the ‘chain of consequences’ during hazard exposure;• Use of scenarios: Assess consequences of 1m inundation;• Compare a worst case scenarios with and without fl ooding;•
Events and circumstances
Undesireable event
Failure trees, hazards
Additional scenarios flooding
flooding
Worst Case ScenarioNo Flooding
Worst Case ScenarioIncluding Flooding
Casualties None/Limited None/LimitedAffected persons (health effects)
1000(~10 health effects)
1000-2000(~100 health effects)
Economic damage 10-100m EUR (plant, down time, claims)
10-100m EUR (plant, down time, claims)
Environmental damage Minor Signifi cantCultural damage None None
BowTie-Model: Propagation of consequences Outcomes (example)
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 21
(PORT) FLOOD DAMAGE ASSESSMENT: OUTCOMES
Wet bulk and infrastructure are sensitive to fl ood risk: societal disruption:Electricity supply (business interruption);• Roads, tunnels and pipes: supply chain disruption;• ICT services.•
Casualties and health:Limited number of casualties;• Flood could increase health impacts: Flood water as a distributor;• Additional impact of fl ood risk is limited;• EP in the order of 1/1000,000.•
Pitfalls:Cumulative risk: multiple plants are fl ooded because of even terrain;• Risk chemical plants depends largely on weather conditions (e.g. wind).•
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 22
3. CONCLUSIONS
FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 23
CONCLUSIONS
Current vulnerability is limited:High level of risk diff erentiation between areas;• Especially historical housing stock protected;• Yet, area is vulnerable to ‘extreme events’• Limited additional risk to Rotterdam port area. Yet, potential for societal disrup-• tion during ‘extreme event’
Climate change:Considerable increase of fl ood impact, especially in urban areas;• Shift in fl ood damages: historic areas (e.g. Dordrecht).•
Further study:Coupling local adaptation measures to diff erent risk profi les;• Assessment of structural/non structural measures (e.g. insurance);• Methodological improvement: damage curves (functional, typological, etc.)• Indirect damages assessment port area: ripple eff ects•
HSRR02FLOODRISKASSESSMENTINUNEMBANKEDAREASINTHENETHERLANDS
September 2010 FLOODRESILIENCEGROUP
Kennis voor Klimaat Knowledge for Climate
Page 24
WATERVEILIGHEID BUITENDIJKS SYNTHESE
FLOOD RISK IN UNEMBANKED AREAS
SYNTHESIS
CONCLUSIONS
More information at: www.kennisvoorklimaat.org•