lee tues 4pm ligurian.pdf
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UsingRobustSimulationtoCharacterize Uncertainties in
CatastropheLoss
Assessments
Yajie J.Lee,CraigE.Taylor,Zhenghui Hu,WilliamP.Graf,
CharlesK.
Huyck
RAACatModeling2014
February1113,2014,Orlando,FL
ImageCat, Inc.
Supportingthe
global
risk
and
disaster
management
needs
of
today,
using
the
technologiesoftomorrow
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EQECatfounded
HAZUS BuildingModels
CloudComputing
Dynamic Financial Analysis
AIRfounded
RMS
founded
-
o ust mu at on
(recognized uncertai
nty)
Determinis tic Cat Scenarios
IBMPCU
sage
Risk Curves ('EP') forsynthetic catalogs
Governmentstudies [Wiggins,
ESSA, Friedman]
Tracking ExposureAccumulations in Zones
Realistic DisasterScenarios
1970 1980 1990 2000 2010 2020San FernandoValley
LomaPrieta
Northridge Tohoku +Christchurch
Algermissen & Perkins Frankel et al Petersen et alUSGS Probabili stic
1996 2002 2008 201419901976
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AFramework
for
More
Robust
Uncertaint
Assessment
RobustSimulation
CurrentApproach
$M)
Amount(
Los
AverageReturnInterval(Years)
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Scientificchallenges
WhatisRobustSimulation?
USGSnationalseismicmaps
g y
Portfoliolosses
Conc usions
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Scientificchallenge:Whatassumptionsaremadeaboutmaximum
events?
BUT!Japanesegeologistshadrecognizedlargereventsinthedecadebeforetheearthquakefromancienttsunamirecords
~ . M9.6couldoccurinanysubductionzones
Thoku wasM9.0,ruptured5segments
(Imagesource: Steinetal.,TectonicPhysics,2012)
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Scientificchallenge:Howaccuratelyareseismicsourcesmapped?
NewMadrid
(USGSNSHM,2014)
M6.8 to M8.0
Reoccurrencemodel
500to50,000years
Cluster &Noncluster
o e au mo e or
nuclearpowerplantPseudofaults
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Scientificchallenge:Howstrongwillthegroundshake?
GMPEsforSubduction Earthquakes(Abrahamson2012)
GMPEsforCEUS(USGS NSHM,2014)
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Scientificchallen e:Howwelldoesabuildin erformduringgroundshaking?
(Forcebasedparadigm)
(Displacementbased
aradi m
(A1970ConcreteFrame)
Increasingbuildingperiods
(CODA:CodeOrientedDamageAssessmentmethod,
adaptedfromATC13,Graf&Lee,Spectra,2009)
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WhatAssum tionsaremadeaboutmissin data?
Lo
ss
Time
Loss
ss
Lo
Time
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,answer?
elihood
Asinglenumber?
Lik
Severity
OrAdistribution
Likelihood basedwhatwenowknow?
Severity
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Scientificchallenge:Howdoweaccountforuncertainty?
Twotypeso mo e e uncertainties
Innermodelrandomness(aleatory)
Givenenoughtime,thevalueswillberealized
afterasufficient
number
of
event
cycles
Outermodelvariation(epistemic)
Lackofknowled e scientific modeluncertaint
Onlytime
or
future
research
will
tell
the
correct
model
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RobustSimulation:Representationoffutureriskthroughsimulationofasuiteofpossibleanswersthatintegratesvalidscientificdisagreementandstochasticmodelingofunknownvariables.
ity
Sever
ReturnInterval
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A licationofrobust
estimation:e sm c azar assessment
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Logic will be more complex in 2014 NSHM models!
2008USGSNationalSeismicHazardMapping(NSHM).
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A site in San Francisco A site in Los Angeles
475year(USGS) 475year(USGS)
1412
0
2
4
6
8
10
12
Count
2 6 .1 4 8 2 6 .3 4 8 2 6 .5 4 8 2 6 .7 4 8 2 6 .9 4 8
0
2
4
6
8
10
Coun
t
0.0
2
0.0
60
.1
0.1
4
0.1
8
0.2
2
0.2
60
.3
0.3
4
0.3
8
0.4
2
0.4
60
.5
0.5
4
0.5
8
0.6
2
0.6
60
.7
0.7
4
0.7
8
0.8
2
0.8
60
.9
0.9
4
0.9
8
PGA (g)
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
PGA (g)
Groundmotiondistributionat475yearreturninterval
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Applicationof
robust
estimation:
singleproperty
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A
sample
mid
rise
office
buildingLosAngeles,1965
Concreteshearwall
Concreteshearwall: 35%
Concreteframe: 17.5%
Steelframe: 17.5%
Woodframe: 10%
Steelconcentricbracedframe: 20%
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Comparisonwith
Federico
Waismans 2010RAAearthquake
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(Waisman,2010)
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ImageCat (ConventionalApproach)
(Waisman,2010)
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ARobustEstimateofUncertainty
RobustSimulation
ConventionalEPcurvent($M
)
LossAmo
AverageReturnInterval(Years)
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ARobustEstimateofUncertainty
nt($M
)
LossAmo
AverageReturnInterval(Years)
UsingmultipleanswersfromvariousCatmodelersdoesnotnecessarily
disclosethefullrangeofuncertaintyinpotentialCatrisks.
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o ust mu at on:
Acce tsmodelim erfection
Acknowledgesmodellimitations
Revealsuncertaintyassociated
with
imperfect
knowledgeEncouragesmodeldivergence
Fewersurprises(Black
Creditordiscreditextreme
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Providesacontrolled
Modeltraceability Preserves coherenc and
integrity
Usesnonparametr cstat st csMinimizesneedforcomplex
classicalstatistics
Propagatesuncertaintythroughlayers,simplifyingcomplex
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Simplifiestimesequenceoflosses
Clusteredevents,e.g.,NMSZ,
Simplifiesmultiperilmodeling
Flood
Winterstorm
EarthquakeTsunami
TerrorThedrunkardswalk
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Asingleviewofrisksuppressesmodeluncertaint andim lies
Thailand
illusoryprecisiontomodelingfutureriskwithmanyunknowns.
Re ulators and modelers havebeguntostressunderstandingmodellimitationsand
uncertainty
Thoku
Uncertaintycanchangewhenmoreinformationisacquired
toassessuncertaintyadequatelyandallocateresourcesaccordin l
Christchurch
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