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International Conference: International Conference: Global Global and Regional Climate Changes and Regional Climate Changes Kyiv, Ukraine Kyiv, Ukraine 16 16 - - 19 Nov, 2010 19 Nov, 2010 Decisionmaking Decisionmaking for Climate for Climate Adaptation in the Water Sector Adaptation in the Water Sector Eugene Z. Stakhiv (3EHOH CTAXIB) UNESCO-ICIWaRM and Institute for Water Resources U.S. Army Corps of Engineers
Transcript

International Conference: International Conference: ““Global Global and Regional Climate Changesand Regional Climate Changes””

Kyiv, UkraineKyiv, Ukraine1616--19 Nov, 201019 Nov, 2010

DecisionmakingDecisionmaking for Climatefor ClimateAdaptation in the Water SectorAdaptation in the Water Sector

Eugene Z. Stakhiv(3EHOH CTAXIB)

UNESCO-ICIWaRMand

Institute for Water ResourcesU.S. Army Corps of Engineers

Transitioning to Transitioning to AdaptationAdaptationunder Climate Uncertaintyunder Climate Uncertainty

How to deal with risk, uncertainty and How to deal with risk, uncertainty and ‘‘unknownsunknowns’’ in decision making?in decision making?WeWe’’re in a re in a 2020--year transition periodyear transition period before before good information and reliable models become good information and reliable models become available.available.How to deal with nonHow to deal with non-- stationary climate?stationary climate?Role of Role of GCMsGCMs in evaluation of water resources in evaluation of water resources management optionsmanagement optionsAre the current methods (i.e. stochastic Are the current methods (i.e. stochastic hydrology) hydrology) ‘‘good enoughgood enough’’ to deal with to deal with uncertainty?uncertainty?Are there practical engineering design methods Are there practical engineering design methods to deal with to deal with ‘‘robustnessrobustness’’, , ‘‘resiliencyresiliency’’ and and ‘‘reliabilityreliability’’ ??

Recent AssessmentRecent Assessment of Climate Modelsof Climate Models

Regional trends in extreme events are not always captured by current models

It is difficult to assess the significance of these discrepancies and to distinguish between model deficiencies and natural variability

How Accurate Are Global Climate Models?

Context for Climate Change and Sustainable Context for Climate Change and Sustainable Development: Levels of Analysis for aDevelopment: Levels of Analysis for aConventional Risk Mgmt FrameworkConventional Risk Mgmt Framework

Sustainable Development(‘Vision’, Goals)

Integrated Water Resources Mgmt(IWRM)

Climate Adaptation(e.g. IFM, IDM, infrastructure)

Adaptive Management(Forecasting, monitoring, modeling)

ClimateChange

IWRIWRManagementManagementof Water Sectorsof Water Sectors

Integrated Drought

Mgmt

IntegratedFlood

Management

Urban Water Supply

EcologicalFlows

Hydro-power

CommercialNavigation

Irrigation& Drainage

Integrated Water Resources Management

Integrated River Basin (Watershed) Management

Water Sector Focus is on Water Sector Focus is on Risk ManagementRisk Management for for Climate VariabilityClimate Variability (which is foundation for CC)(which is foundation for CC)

Design, operations, rehabilitation require project Design, operations, rehabilitation require project evaluation & design criteria: combination of standards evaluation & design criteria: combination of standards & risk analysis& risk analysisDam safety (convert PMP/PMF to riskDam safety (convert PMP/PMF to risk--based designs)based designs)Levee design criteria ( SPF to riskLevee design criteria ( SPF to risk--based designs)based designs)Shore erosion, coastal protection (PMH)Shore erosion, coastal protection (PMH)Reservoir operating criteria, improved forecastingReservoir operating criteria, improved forecastingReservoir/system water allocation changesReservoir/system water allocation changesDelineation of 100Delineation of 100--year floodplains/NFIPyear floodplains/NFIPDrought & Flood Contingency Mgmt (reservoir, urban)Drought & Flood Contingency Mgmt (reservoir, urban)Emergency Operations/Advanced Measures (seasonally Emergency Operations/Advanced Measures (seasonally anticipated snowmelt flooding, hurricanes, etc.)anticipated snowmelt flooding, hurricanes, etc.)

In In transition period,transition period, need new/extended methods for need new/extended methods for flood/drought frequency analysis under nonflood/drought frequency analysis under non--stationary stationary climate, with trends.climate, with trends.

Different methods for incorporating Different methods for incorporating Climate Information into Water Climate Information into Water Sector Project Planning/DesignSector Project Planning/Design

GCM scenario analysisGCM scenario analysis (test plans for (test plans for robustness, resiliency, reliability)robustness, resiliency, reliability)Traditional Traditional Stochastic analysisStochastic analysis of historic of historic datadataHindcastingHindcasting based on based on dendroclimatologydendroclimatology& statistical & statistical ‘‘voodoovoodoo’’ to extend records to extend records Extending Extending existing statistical tools & existing statistical tools & modelsmodels (e.g. LP3 (e.g. LP3 ‘‘fatfat--tailedtailed’’ distribdistrib--GEV)GEV)GCM downscalingGCM downscaling and derived frequency and derived frequency analysis (not ready for analysis (not ready for ‘‘prime timeprime time’’).).

Conventional Mechanisms for Adapting to Conventional Mechanisms for Adapting to Climate UncertaintiesClimate Uncertainties

Planning Planning new investmentsnew investments, or for capacity expansion , or for capacity expansion (reservoirs, irrigation systems, levees, water supply, (reservoirs, irrigation systems, levees, water supply, wastewater treatment)wastewater treatment)Operation & regulationOperation & regulation of existing systems: of existing systems: accommodating new uses or conditions (e.g. ecology, accommodating new uses or conditions (e.g. ecology, climate change, population growth)climate change, population growth)Maintenance and Maintenance and majormajor rehabilitationrehabilitation of existing of existing systems (e.g. dams, barrages, irrigation systems, systems (e.g. dams, barrages, irrigation systems, canals, pumps, etc.)canals, pumps, etc.)Modifications in Modifications in processes and demandsprocesses and demands (water (water conservation, pricing, regulation, legislation)conservation, pricing, regulation, legislation)Introduce new Introduce new efficient technologiesefficient technologies (desalting, (desalting, biotechnology, drip irrigation, wastewater reuse, biotechnology, drip irrigation, wastewater reuse, recycling, solar energy )recycling, solar energy )

Functions/Elements of Water Resources Management

Corps Reservoir Operations:Corps Reservoir Operations:Revising/Updating RegulationsRevising/Updating Regulations

Reservoir Master manual

Emergency Operations[ER 11-1-320]

Standard ProjectFloods

[EM 1110-2-1411]

Inflow Design Floods

[ER-1110-8-2]

Review of Completed Projects

[ER 1105-2-100;ER 1165-2-119]

Dam Safety Assurance Program

[ER 1110-2-1155]

Management of Water Control

Systems[EM 1110-2-3600]

Water ControlManagement[ER 1110-2-240]

Drought ContingencyPlans

[ER 1110-2-1941

Corps’ Dam Safety Portfolio Risk Management Process

Risk Informed Priorities for Permanent Risk Reduction

Tolerable Risk Guidelines

Interim Risk Reduction Measures

Issue Evaluation Studies

Dam Safety Modification Reports

Periodic Inspections/Periodic

Assessments/Asset Management

National Dam Safety Program

Routine Inspections: Verifies O&M, More Rigorous Standards, Improved Communication, System-based, Every Year

Periodic Inspections:Verifies O&M, Evaluates Structure Stability, Compares Constructed Criteria to Current Criteria, Every 5 Years

Risk Assessments:Data Intensive, Determine Likelihood and Consequences of Failure, Every 10 Years

Increasing Rigor

Periodic Assessments:Periodic Inspection + Potential Failure Mode and Consequences Analysis, Every 5 Years

Levee Screening: Begin to categorizing.

National Levee Safety Program

Continuous Feedback

Mission: Assess integrity and viability of levees, recommend actions to assure levee systems do not present unacceptable risks to public, property, environment.

11 Water Oriented Agencies11 Water Oriented AgenciesMeet quarterly to align and unify federal Meet quarterly to align and unify federal

floodplain and risk management floodplain and risk management programs and issuesprograms and issues

ReRe--instituted September 2009instituted September 2009Developing fiveDeveloping five--year work planyear work planConducting public listening sessionsConducting public listening sessionsDrafting updated Executive Order Drafting updated Executive Order

governing floodplain managementgoverning floodplain management

Federal Interagency Floodplain Management Task Force

16th century “megadrought”>100 year “megadroughts”

2000-year Climate history of central U.S.

DustBowl

2000 yrs. ago Today

Source: Overpeck 2004

The US Breadbasket: The Mid-West

Uncertainty and Flood Damage CalculationUncertainty and Flood Damage Calculation(Corps of Engineers Procedures (Corps of Engineers Procedures -- HECHEC--FDA;1992)FDA;1992)

Floo

d St

age

(S)

Floo

d St

age

(S)

Flood Discharge (Q)

Flood Discharge (Q)

Freq

uenc

y

Freq

uenc

y

Flood Damage (D)

Flood Damage (D)

Q

S

P

Q

P

D

S

D

UEB - Upper Error Bound

LEB - Lower Error Bound

UEB

LEB

ENSO Floods: LP3 distributionENSO Floods: LP3 distributionMississippi River at Hannibal, Missouri

10000

100000

1000000

-3 -2 -1 0 1 2 3 4

Cumulative Probability (in Units of Standard Deviation)

Dis

char

ge (c

fs)

Log Pearson III Other Floods El Nino Floods

1993 Flood

R&U Flood Damages AnalysisR&U Flood Damages Analysis

Discounted Discounted AvgAvg Annual Net Annual Net Benefits (Benefits Benefits (Benefits –– Costs)Costs)

0.95

(25.0)

(40.0)

(155.0)

(30.0)

(20.0)

(300.0)

LongLong--term Risk of Failure term Risk of Failure

Uncertainty and Flood Damage CalculationUncertainty and Flood Damage Calculation(Corps of Engineers Procedures (Corps of Engineers Procedures -- HECHEC--FDA;1992)FDA;1992)

Floo

d St

age

(S)

Floo

d St

age

(S)

Flood Discharge (Q)

Flood Discharge (Q)

Freq

uenc

y

Freq

uenc

y

Flood Damage (D)

Flood Damage (D)

Q

S

P

Q

P

D

S

D

UEB - Upper Error Bound

LEB - Lower Error Bound

UEB

LEB

Hydrologic Hydrologic ExcedanceExcedance graph graph

0.0000

0.2000

0.4000

0.6000

0.8000

1.0000

1.2000

0 5000 10000 15000 20000 25000 30000 35000

Discharge (cfs)

Exce

edan

ce GEVLP3GumbelData

Discharge Recurrence Intervals for Different Discharge Recurrence Intervals for Different Frequency Distributions:Frequency Distributions:

100100--year event GEV distribution = 225year event GEV distribution = 225--year event on LP3year event on LP3

0

5000

10000

15000

20000

25000

30000

35000

0 50 100 150 200

Recurrence Interval (years)

Disc

harg

e (c

fs)

GEVLP3Gumbel

CONCLUSIONSCONCLUSIONSFlood and Drought Management are the Flood and Drought Management are the ‘‘leading edgeleading edge’’of any pragmatic adaptation strategy of any pragmatic adaptation strategy –– both for both for ‘‘managedmanaged’’ and and rainfedrainfed systems.systems.Stochastic hydrology is still a useful way of dealing Stochastic hydrology is still a useful way of dealing with climate uncertaintywith climate uncertaintyThe best way to deal with uncertainty is to use proven The best way to deal with uncertainty is to use proven engineering design methods to upgrade engineering design methods to upgrade resiliency,resiliency,robustness and reliability,robustness and reliability,IWRM is the accepted paradigm/context for dealing IWRM is the accepted paradigm/context for dealing with climate adaptation and adaptive managementwith climate adaptation and adaptive managementTransitional pragmatic economic evaluation and Transitional pragmatic economic evaluation and engineering design tools needed in absence of good engineering design tools needed in absence of good information from information from GCMsGCMs and forecasting modelsand forecasting modelsExpansion and improvement of current Expansion and improvement of current hydromethydrometmonitoring systems is essential to effective climate monitoring systems is essential to effective climate adaptation adaptation –– espesp adaptive managementadaptive managementEconomic decision criteria dominate any adaptation Economic decision criteria dominate any adaptation responses responses –– need to be revisedneed to be revised

Finis-Merci

1 0.5 0.2 0.1 0.05 0.02 0.01 0.005 0.002 0.001 Probability of Exceedance

Return Period (Years)1 2 5 10 20 50 100 200 500 1000

600

500

400

300

200

100

0

Dis

char

ge(1

000

cfs)

Potential Hydrologic Scenarios 1. Precipitation and Runoff Trends 1. Precipitation and Runoff Trends

(e.g. (e.g. increase/decreaseincrease/decrease))2. Hydrologic Variability 2. Hydrologic Variability

(e.g. (e.g. magnitude/severity/durationmagnitude/severity/duration))

Higher Mean

Lower Mean

Higher Variability

Lower Variability

Climate ModelGrid-Scale

GCM

RCM

DS

Dow

nscaling

Land

Aggr

egat

ion

Vegetation

Precipitation

Topography

Climate Model Downscaling to watershed Scale

Prec

ipita

tion

pred

ictio

n

Time (years)Present Future 20 40 60 80

Climate Model Downscaling to Regional/Watershed ScalesGeneration of Future Precipitation Scenarios: Single Model – Multiple Realization

Multi-Model Ensemble Approach Generation of Future Precipitation Scenarios

INTERFLOWSURFACERUNOFF

INFILTRATIONTENSION

TENSION TENSION

PERCOLATION

LOWERZONE

UPPERZONE

PRIMARYFREE

SUPPLE-MENTAL

FREE

RESERVED RESERVED

FREE

EVAPOTRANSPIRATION

BASEFLOW

SUBSURFACEOUTFLOW

DIRECTRUNOFF

Precipitation

Present Future 20 40 60 80Time (years)

Prec

ipita

tion

pred

ictio

n

Present Future Time (years)

Flo

wGeneration of Future Runoff Scenarios

Downscaled Precipitation to Runoff Generation

Climate ModelGrid-Scale

GCM

RCM

DS

Dow

nscaling

Land

Aggr

egat

ion

Vegetation

Precipitation

Topography

Climate Model Downscaling to regional/watershed Scale

A Valid Question to Ask: Given the Current State of Climate Models (especially at

regional scales) , What is the added-value of all the Downscaling Studies over traditional statistical hydrology methods in water resources studies?

Probability density function

Time (years)Present

Future

10 20 30 40 50 60 70 80 90 100 -100 -75 -50 -25 0

Flo

w (

m3 /s

ec)

Past

0255075100125150175200225250

1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 2000Flo

w (m

3 /sec

)Time (years)

Statistical Hydrology: “synthetic” stream flow Generation

1 0.5 0.2 0.1 0.05 0.02 0.01 0.005 0.002 0.001 Probability of Exceedance

Return Period (Years)1 2 5 10 20 50 100 200 500 1000

600

500

400

300

200

100

0

Dis

char

ge(1

000

cfs)

Potential Hydrologic Scenario: Stationarity!

Sept 1951 Elephant Butte, NM Jan 2003Middle Rio Grande Basin, NM AD Grissino-Mayer, Baisan,

Morino, & Swetnam, 2001

Statistical Hydrology Developed Based on Stationarity Assumption

1250 1350 1450 1550 1650 1750 1 850 1950 2050 2150 2250 2350 2450 2550 2650 2750

Rec

onst

ruct

ed P

DSI

---------

2.0

1.5

1.0

0.5

0

-0.5

-1.0

-1.5

-2.0

Past Present Future

Wide-Range of Impacts on Infrastructure Design

•Presently, the accuracy of regional-scale climate model fall short of meeting the requirements of water resources planning.

• The value of Traditional stochastic hydrologymethods should not be underestimated. Research is required to advance their capability to address Hydroclimate decision making needs.

Concluding points

Factoring in Resiliency in water resources systems design and planning is still the safest approach!

NOAA: El NiNOAA: El Niñño to Help Steer U.S. o to Help Steer U.S. Winter Weather (Winter Weather (October 15, 2009)October 15, 2009)

NOAA Highlights of the U.S. Winter Outlook NOAA Highlights of the U.S. Winter Outlook (December through February) include:(December through February) include:

WarmerWarmer--thanthan--average temperaturesaverage temperatures are favored across much of the western are favored across much of the western and central U.S., especially in the northand central U.S., especially in the north--central states from Montana to central states from Montana to

Wisconsin. Though temperatures may average warmer than usual, peWisconsin. Though temperatures may average warmer than usual, periodic riodic outbreaks of cold air are still possible. outbreaks of cold air are still possible.

BelowBelow--average temperaturesaverage temperatures are expected across the Southeast and midare expected across the Southeast and mid--Atlantic from southern and eastern Texas to southern PennsylvaniAtlantic from southern and eastern Texas to southern Pennsylvania and south a and south

through Florida. through Florida. AboveAbove--average precipitationaverage precipitation is expected in the southern border states, is expected in the southern border states,

especially Texas and Florida. Recent rainfall and the prospects especially Texas and Florida. Recent rainfall and the prospects of more should of more should improve current drought conditions in central and southern Texasimprove current drought conditions in central and southern Texas. However, . However,

tornado records suggest that there will also be an increased chatornado records suggest that there will also be an increased chance of organized nce of organized tornado activity for the Gulf Coast region this winter. tornado activity for the Gulf Coast region this winter.

DrierDrier--thanthan--averageaverage conditions are expected in the Pacific Northwest and the conditions are expected in the Pacific Northwest and the Ohio and Tennessee River Valleys. Ohio and Tennessee River Valleys.

NortheastNortheast: Equal chances for above: Equal chances for above--, near, near--, or below, or below--normal temperatures and normal temperatures and precipitation. Winter weather in this region is often driven notprecipitation. Winter weather in this region is often driven not by El Niby El Niñño but by o but by weather patterns over the northern Atlantic Ocean and Arctic, suweather patterns over the northern Atlantic Ocean and Arctic, such as the North ch as the North Atlantic Oscillation. These patterns are often more shortAtlantic Oscillation. These patterns are often more short--term, and are generally term, and are generally

predictable only a week or so in advance. predictable only a week or so in advance. California:California: A slight tilt in the odds toward wetterA slight tilt in the odds toward wetter--thanthan--average conditions over average conditions over

the entire state. the entire state. Alaska:Alaska: MilderMilder--thanthan--average temperatures except along the western coast. Equal average temperatures except along the western coast. Equal chances for abovechances for above--, near, near--, or below, or below--median precipitation for most areas except median precipitation for most areas except

above median for the northwest. above median for the northwest. Hawaii:Hawaii: BelowBelow--average temperatures and precipitation are favored for the entiraverage temperatures and precipitation are favored for the entire e

state.. state.. This seasonal outlook does not predict where and when snowstormsThis seasonal outlook does not predict where and when snowstorms may hit or may hit or

total seasonal snowfall accumulations. Snow forecasts are dependtotal seasonal snowfall accumulations. Snow forecasts are dependent upon winter ent upon winter storms, which are generally not predictable more than several dastorms, which are generally not predictable more than several days in advance.ys in advance.

If you canIf you can’’t make t make sense of the GCM sense of the GCM scenariosscenarios……If you canIf you can’’t rely on t rely on

seasonal forecastsseasonal forecasts……If your predictions of If your predictions of

hurricane activity have hurricane activity have failed, then tryfailed, then try……..

2010 Farmers’Almanac Predictions for the U.S.

Uncertainty and Flood Damage CalculationUncertainty and Flood Damage Calculation(Corps of Engineers Procedures (Corps of Engineers Procedures -- HECHEC--FDA;1992)FDA;1992)

Floo

d St

age

(S)

Floo

d St

age

(S)

Flood Discharge (Q)

Flood Discharge (Q)

Freq

uenc

y

Freq

uenc

y

Flood Damage (D)

Flood Damage (D)

Q

S

P

Q

P

D

S

D

UEB - Upper Error Bound

LEB - Lower Error Bound

UEB

LEB

How to translate Global Warming How to translate Global Warming GCM Info into real decisions?GCM Info into real decisions?

Top down approach Top down approach (advocated by (advocated by climate modeling community)climate modeling community):: translating translating GCM outputs into design criteria and GCM outputs into design criteria and decisions, assuming that information is decisions, assuming that information is useful and certainuseful and certainBottom Up:Bottom Up: (advocated by the (advocated by the practitioners) develop incremental practitioners) develop incremental adaptive coping strategies based on adaptive coping strategies based on engrgengrgpractice and experience with risk, practice and experience with risk, uncertainty and build in resiliency, uncertainty and build in resiliency, robustness and reliability (just as werobustness and reliability (just as we’’ve ve always done from the times of the always done from the times of the PharaohsPharaohs

Hurricanes & Global Warming?Hurricanes & Global Warming?2004, 2005 Atlantic hurricane seasons broke 2004, 2005 Atlantic hurricane seasons broke many recordsmany records2006 predicted to have 15 named storms; 10 2006 predicted to have 15 named storms; 10 hurricane strength; 4hurricane strength; 4--5 major making 5 major making landfall in US landfall in US 2006 A BUST !!! Not much happened (FEMA, 2006 A BUST !!! Not much happened (FEMA,

Corps and other agencies spent $millions Corps and other agencies spent $millions anticipating) 2007, 2008, 2009 as well.anticipating) 2007, 2008, 2009 as well.Debate among US meteorologists:Debate among US meteorologists:

A. 25A. 25--40 yr cycle ?40 yr cycle ? (e.g. (e.g. LandseaLandsea & Gray) or & Gray) or B. part of global warming cycleB. part of global warming cycle ?? (e.g. (e.g.

Emmanuel) Emmanuel) Herein lies the problem for water engineersHerein lies the problem for water engineers-- how to how to

translate vague climate scenarios, scientific disputes translate vague climate scenarios, scientific disputes and flawed predictions into design criteria for reliable and flawed predictions into design criteria for reliable structures and response systems?structures and response systems?

0

5

10

15

20

25

30

1854

1858

1862

1866

1870

1874

1878

1882

1886

1890

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1898

1902

1906

1910

1914

1918

1922

1926

1930

1934

1938

1942

1946

1950

1954

1958

1962

1966

1970

1974

1978

1982

1986

1990

1994

1998

2002

Total number of tropical cyclones

Number of hurricanes

Number of hurricanes which center's madeU.S. landfall

Source: National Oceanic & Atmospheric Administration

Note: Prior to 1970, tropical cyclones were not monitored by satellites; meaning that those cyclones that did not hit the land of the United States were not systematically recorded.

MANY STRONG WEAKER MANY STRONG WEAKER

Cycle of Hurricanes* (James O’Brien)

Most Damaging HurricanesMost Damaging HurricanesYear Cat Year Cat

DamagesDamagesKatrina (FL, LA, MS) 2005 3+ $ Katrina (FL, LA, MS) 2005 3+ $ 100.0 B +100.0 B +Andrew (FL, LA) 1992 5 Andrew (FL, LA) 1992 5 43.6 B43.6 BCharley (FL) Charley (FL) 2004 42004 415.0 B15.0 BIvan (AL, FL) Ivan (AL, FL) 2004 32004 314.2 B14.2 BHugo (SC) 1989 4 Hugo (SC) 1989 4 12.2 B12.2 BAgnes (FL, GA, SC, PA) 1972 2 Agnes (FL, GA, SC, PA) 1972 2 11.3 B11.3 B

Flood Damages as Percent of GDP(Based on damages and GDP data in 2000 dollars)

0.0%

0.1%

0.1%

0.2%

0.2%

0.3%

0.3%

0.4%

0.4%

0.5%

0.5%

1900

1903

1906

1909

1912

1915

1918

1921

1924

1927

1930

1933

1936

1939

1942

1945

1948

1951

1954

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1972

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1978

1981

1984

1987

1990

1993

1996

1999

2002

2005

Dir

ect f

lood

dam

ages

as

perc

ent o

f GD

P

0%

5%

10%

15%

20%

25%

Tota

l flo

od d

amag

es a

s pe

rcen

t of G

DP

Direct damages as percent of GDPTotal damages as percent of GDP

MississippiRiver Valley

Ohio & Lower Mississippi River

Basins

Kansas &Missouri Rivers

HurricaneDiane

Hurricane Agnes

Teton DamFailure

Midwest Floods

138%

61%

99%

Floods in Floods in a a

changing changing climateclimate

Nature, 2002

Or Not Or Not …… Kundzewicz et al., 2005

Spatial Comparison

Mean temperature change

73.5

74.0

74.5

75.0

75.5

76.0

1860

1863

1866

1869

1872

1875

1878

1881

1884

1887

1890

1893

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1902

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2001

Lake Ontario Water LevelsLake regulation scenario

IJC Lake Ontario Study:IJC Lake Ontario Study:HHydrologydrologicic Scenarios Including Scenarios Including

Climate ChangeClimate Change

Candidate Plans:Candidate Plans:•• A: Balanced EconomicsA: Balanced Economics•• B: Balanced EnvironmentalB: Balanced Environmental•• D: Blended BenefitsD: Blended Benefits

Natural Flow PlanNatural Flow Plan•• E: Natural Flow E: Natural Flow

Interest Specific:Interest Specific:•• Ontario Riparian PlanOntario Riparian Plan•• Recreational Boating PlanRecreational Boating Plan

Reference Plans:Reference Plans:•• Plan 1998Plan 1998•• Plan 1958DDPlan 1958DD•• Plan 1958DPlan 1958D

IJC International Lake Ontario –St. Lawrence River Study

Bluff Recession for Different Plans (same wave climate)

-2

0

2

4

6

8

10

700 720 740 760 780 800 820

Distance (m)

Blu

ff He

ight

(m)

Climate 2090 1998 Plan 1958D without Dev. Input ProfileClimate 2050 Actual (1966-1995) Pre-Project LWD (m)

Net Economic/Ecologic Benefits Net Economic/Ecologic Benefits of Alternative Plansof Alternative Plans

Avg. annual Avg. annual net benefits net benefits ($US million)($US million) Plan Plan

58DD58DD Plan APlan A Plan BPlan B Plan DPlan D Plan EPlan E

Net BenefitsNet Benefits 0.000.00 7.527.52 6.486.48 6.526.52 --12.3012.30

Shoreline Shoreline DamagesDamages 0.000.00 --0.620.62 --1.111.11 0.320.32 --25.9625.96

NavigationNavigation 0.000.00 0.410.41 2.202.20 2.312.31 4.134.13

Recreation BoatingRecreation Boating 0.000.00 4.234.23 --0.580.58 2.042.04 --4.644.64

HydroelectricHydroelectric 0.000.00 3.503.50 5.975.97 1.821.82 14.1614.16

Municipal WaterMunicipal Water 0.000.00 0.000.00 0.000.00 0.000.00 0.000.00

Environmental Environmental IndexIndex 1.001.00 1.061.06 1.351.35 1.101.10 4.044.04

Wetlands Wetlands IndexIndex 1.001.00 1.021.02 1.441.44 1.171.17 1.561.56

GCM Scenarios:GCM Scenarios: Economic Robustness of PlansEconomic Robustness of PlansIJC Lake OntarioIJC Lake Ontario--St. Lawrence Regulation St. Lawrence Regulation

w.r.t w.r.t Climate Change ScenariosClimate Change Scenarios

--21.3821.389.659.6511.7811.788.338.3313.9813.98C4 C4 -- Warm/WetWarm/Wet

--2.462.4617.7717.772.612.6121.5321.53--81.6981.69C3 C3 -- Hot/WetHot/Wet

--34.0334.035.255.254.894.899.859.85--49.5249.52C2 C2 -- Warm/DryWarm/Dry

--4.914.9120.0920.09--1.421.4234.8934.89--115.65115.65C1C1-- Hot/DryHot/Dry

--12.3012.306.526.526.486.487.527.5200Plan 1958DDPlan 1958DD(current plan)(current plan)

Econ Econ Environ Combo NaturalEnviron Combo NaturalEfficiency QuEfficiency Quality Benefits Flowsality Benefits Flows

Plan EPlan EPlan DPlan DPlan BPlan BPlan APlan APlanPlan

1958DD1958DD

Avg. ann. Avg. ann. net benefits net benefits ($US million)($US million)

Ecological Robustness/ResiliencyEcological Robustness/Resiliency-- Stochastic ScenariosStochastic Scenarios

(# Ecological Performance (# Ecological Performance IndicatorsIndicators’’ss (of 32) with gains or losses)(of 32) with gains or losses)

-10

-5

0

5

10

15

20

Plan A

Net

# o

f PIs

w/ S

igni

fican

t Gai

ns

Historical (1900-2000)Stochastic #1 - Wettest CenturyStochastic #2 - Driest CenturyStochastic #3 - Like HistoricalStochastic #4 - Longest Drought

Plan A Plan D Plan B PreProject

Hydro-Dendro-Climatology

Hindcasting the Flood Record with “Voodoo” Statistical Analysis

The The ‘‘Double DiscountDouble Discount’’ Dilemma of Dilemma of Water Project JustificationWater Project Justification

In the classical expected-value approach, extreme events with low probability of occurrence are given the same proportional weight/importance (in the multiobjective

commensuration process) regardless of theirpotential catastrophic or irreversible impact.

Discounting for the present value of future benefits (r= discount rate of 2, 5, 7, 10 %)Discounting of low probability, high consequence events using flood/drought frequency analysis for ‘expected annual damages’

Effect of Discount Rate on Choice of Option Effect of Discount Rate on Choice of Option for Protection against Sea Level Rise for Protection against Sea Level Rise

0.02 0.03 0.04 0.05 0.06 0.07 0.08(20)

0

20

40

60

80

Discount Rate

Net

Pre

sent

Val

ue ($

'000

,000

)

Project A Project B

Project ANo SLR

Project BWith SLR

Most Damaging HurricanesMost Damaging HurricanesYear Year Cat Cat DamagesDamages

Katrina (FL, LA, MS) 2005 3+ $ 100.0 B +Katrina (FL, LA, MS) 2005 3+ $ 100.0 B +Andrew (FL, LA) 1992 5 43.6 BAndrew (FL, LA) 1992 5 43.6 BCharley (FL) Charley (FL) 2004 42004 4 15.0 B15.0 BIvan (AL, FL) Ivan (AL, FL) 2004 32004 3 14.2 B14.2 BHugo (SC) 1989 4 12.2 BHugo (SC) 1989 4 12.2 BAgnes (FL, GA, SC, PA) 1972 2 11.3 BAgnes (FL, GA, SC, PA) 1972 2 11.3 BBetsy (FL, LA) 1965 3 10.8 BBetsy (FL, LA) 1965 3 10.8 BFrances (FL) Frances (FL) 2004 22004 2 8.9 B8.9 BCamille (MS, LA, VA) 1969 5 8.9 BCamille (MS, LA, VA) 1969 5 8.9 BDiane (East Coast) 1955 1 6.9 BDiane (East Coast) 1955 1 6.9 BJeanne (FL) Jeanne (FL) 2004 32004 3 6.9 B6.9 B

Flood Damages as Percent of GDP(Based on damages and GDP data in 2000 dollars)

0.0%

0.1%

0.1%

0.2%

0.2%

0.3%

0.3%

0.4%

0.4%

0.5%

0.5%

1900

1903

1906

1909

1912

1915

1918

1921

1924

1927

1930

1933

1936

1939

1942

1945

1948

1951

1954

1957

1960

1963

1966

1969

1972

1975

1978

1981

1984

1987

1990

1993

1996

1999

2002

2005

Dir

ect f

lood

dam

ages

as

perc

ent o

f GD

P

0%

5%

10%

15%

20%

25%

Tota

l flo

od d

amag

es a

s pe

rcen

t of G

DP

Direct damages as percent of GDPTotal damages as percent of GDP

MississippiRiver Valley

Ohio & Lower Mississippi River

Basins

Kansas &Missouri Rivers

HurricaneDiane

Hurricane Agnes

Teton DamFailure

Midwest Floods

138%

61%

99%

WeWe’’re in a Transitional Period of Many re in a Transitional Period of Many Climate Uncertainties and UnknownsClimate Uncertainties and Unknowns

Basic Messages:Basic Messages:All drivers of hydrological cycle are affected by climate All drivers of hydrological cycle are affected by climate variability (CV) & global warming variability (CV) & global warming –– climate change climate change (CC)(CC)Water sector is the principal medium through which Water sector is the principal medium through which most people will experience CCmost people will experience CCMany tools, water resources management coping Many tools, water resources management coping options designed for Climate Variability (CV), form the options designed for Climate Variability (CV), form the foundations for CC adaptationfoundations for CC adaptationSocioeconomic factors, land uses, conflicts and Socioeconomic factors, land uses, conflicts and population dynamics will dominate future conditions & population dynamics will dominate future conditions & and modes of adaptation and modes of adaptation -- rather than CCrather than CCTherefore, CC adaptation must be cast within a broader Therefore, CC adaptation must be cast within a broader IWRM frameworkIWRM framework, & not viewed as an independently , & not viewed as an independently pursued analytical paradigm focusing only on CCpursued analytical paradigm focusing only on CCImproving water governance and management is key Improving water governance and management is key to CC adaptation, more so than GCM to CC adaptation, more so than GCM modellingmodelling

Transitional period (ContTransitional period (Cont’’d)d)Keystone for adaptationKeystone for adaptation and adaptive and adaptive management is a greatly expanded and improved management is a greatly expanded and improved hydromethydromet system for monitoring, modeling and system for monitoring, modeling and forecastingforecastingIntegrated Flood Management (IFM) and Integrated Flood Management (IFM) and Integrated Drought Mgmt (IDM) are the Integrated Drought Mgmt (IDM) are the ‘‘leading edgeleading edge’’ and core of any climate adaptation and core of any climate adaptation strategy for the water sector, and will depend on strategy for the water sector, and will depend on shortshort--term forecasting capabilitiesterm forecasting capabilitiesClimate information, Climate information, GCMsGCMs and prediction services and prediction services need to be need to be dramatically improveddramatically improved before they before they are of value to water managers are of value to water managers Huge upfront investments to avoid highly uncertain Huge upfront investments to avoid highly uncertain and largely unknown CC risks are problematic at and largely unknown CC risks are problematic at this time this time –– but there are sensible methods to but there are sensible methods to accommodate most of these issues in a wellaccommodate most of these issues in a well--organized organized risk management frameworkrisk management framework


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