exercise 6 rick city landslides 2008
DESCRIPTION
Rick City LandslidesTRANSCRIPT
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
RiskCityRiskCityExercise 5:Exercise 5:
Landslide risk assessment. Landslide risk assessment.
Cees van WestenUnited Nations University – ITC School for Disaster Geo-Information
ManagementInternational Institute for Geo-Information Science and Earth Observation (ITC)
Enschede, The NetherlandsE-mail: [email protected]
Associated Institute of the
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Landslide risk exerciseLandslide risk exercise
Three approaches will be done:• Qualitative landslide risk assessment• Semi quantitative • Quantitative
Input data
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Simple vulnerability assessmentSimple vulnerability assessment
Vuln_buildings:=iff(nr_buildings<5,”Low_v”,iff(nr_buildings<25, “Moderate_v”, ”High_v”))
This is of course a large simplification. If more time was available the vulnerability could be better evaluated using Spatial Multi Criteria Evaluation with many more criteria.
Mapping units
Vulnerability
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Qualitative risk assessmentQualitative risk assessmentQualitative_risk = Qualitative_risk [Susceptibility,Vulnerability]
Vulnerability
Susceptibility
Two dimensional table
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Semi-quantitative risk assessmentSemi-quantitative risk assessmentIt combines the susceptibility zones with the mapping units, and calculates the number of houses and people in High, Moderate and Low susceptibility zones
Number of buildings
Risk formula:
Risk =H*V*A
H= Hazard V= VulnerabilityA= Amount of Elements at risk
Risk formula:
Risk =H*V*A
H= unknown V= unknownA= Amount of Elements at risk
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Calculate Nr of buildingsCalculate Nr of buildingsCalculates the number of houses in High, Moderate and Low susceptibility zones
Total area of each mapping unit
Fraction of each unit with high, moderate and low susceptibility
Table mapping units
Table joinCross
Mapping units Susceptibility
LS_Risk_high = LSS_high * nr_buildings
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Calculate Nr of buildingsCalculate Nr of buildings
2699 buildings
7193buildings
16739buildings
The results obtained so far can be a bit misleading because the losses are shown per mapping unit, and not for individual buildings located in high hazard areas.
The number of buildings per mapping units were estimated earlier when a building footprint map was still not available
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Better estimation using Building mapBetter estimation using Building mapCalculates the number of houses in High, Moderate and Low susceptibility zones using Building map
Total area of each mapping unit
Fraction of each unit with high, moderate and low susceptibility
Results using mapping units
Table joinCross
Building map Susceptibility
2699 buildings
4426 buildings
7193buildings
9645buildings
16739buildings
22019buildings
Results using Building map
Cross
High Moderate Low
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Quantitative risk assessmentQuantitative risk assessment
4426 buildings
9645buildings
22019buildings
Risk = Hazard * Vulnerability * Amount How much percentage of the high, moderate and low
hazard classes may be affected by landsides? In which period will these landslides occur? What is the vulnerability to landslides?
Results using mapping unitsHigh Moderate Low
Known nowStill to doOnly susceptibility
Hazard = Spatial probability * Temporal probability
The temporal probability that landslides may occur due to a triggering event. Here we will link the return period of the triggering event with the landslides that are caused by it. We have differentiated return periods of: 50, 100, 200, 300 and 400 years.
The spatial probability that a particular area would be affected by landslides of the given temporal probability. This is calculated as the landslide density within the landslide susceptibility class.
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
From susceptibility to hazardFrom susceptibility to hazardMillion dollar information!!!
Landslide related to different return periods
Landslide_ID map If the indication of the high, moderate and low areas susceptibility is correct, different landslide events with different return periods will give different distributions of landslides in these classes.
The probability can be estimated by multiplying the temporal probability (1/return/period for annual probability) with the spatial probability (= what is the chance that 1 pixel is affected)
Susceptibility
Cross
Density in high
Density in moderate
Density in low
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Calculating hazardCalculating hazardAssumption is that events with a larger return
period will also trigger those landslides that would be triggered by events from smaller return periods
Susc
eptib
ility
cla
sses
Return periods
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Calculating VulnerabilityCalculating VulnerabilitySimple assumption:
The more buildings there are with 3 floors or higher, the lower will be the landslide vulnerability, as it becomes less likely that large buildings will be
destroyed by landslides.
Vuln:=iff(PerVacant=1,0,1-(Perc3floor+Percover3floor))
Estimating landslide vulnerability is very complex.
It requites knowledge on the building types and on the expected landslide volumes and velocities.
These are difficult to estimate. In many study landslide vulnerability of
buildings is simply taken as 1, assuming complete destruction of the elements at risk.
This would, however, in our case give too exaggerated values of risk.
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Calculate lossesCalculate losses
Loss_50_high:=0.0181*vuln*nr_b_highLoss_50_moderate:= 1.31199E-06*vuln*nr_b_moderateLoss_50_low:= 5.96345E-07*vuln*nr_b_lowetc
Losses = Spatial Probability * Consequences Losses = Spatial P * V * A
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Calculate lossesCalculate losses
What can you conclude when you compare the spatial probabilities and consequences for the high, moderate and low susceptibility classes ?
Losses for a return period = sum of losses in high, moderate and low susceptibility areas
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Calculate riskCalculate riskPeriod
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Triangles and Triangles and rectangles rectangles
methodmethod
• The area under the curve is divided into trangles, which connect the straight lines between two points in the curve and have X-axis difference as difference between the losses of the two scenarios. Y-axis of the triangles is the difference in probability between two scenarios. The remaining part under the curve is then filled up with rectangles, as illustrated in the graph and table below.
This is the annual risk, taking the sum of the triangles and squares in the graph
International Institute for Geo-Information Science and Earth Observation (ITC)
ISL 2004
Cost / benefit analysisCost / benefit analysis• Defining risk reduction scenarios• Calculate investment costs• Calculate operation and
maintenance• Define project lifetime• Calculate Net Present Value• Calculate Internal Rate of Return