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Mekong Environmental Symposium | HCMC | 05-07 March 2013 Mekong Environmental Symposium | HCMC | 05-07 March 2013 1
Integrated flood risk assessment for the Mekong Delta
- combined assessment of flood hazard change and social
vulnerability
Heiko Apel1, Matthias Garschagen2, Jose Miguel Delgado1, Nguyen Viet Dung1,3, Vo Van Tuan4, Nguyen Thanh Binh4, Torsten Welle2, Tobias Blätgen2,
Joern Birkmann2, and Bruno Merz1
1 GFZ German Research Centre for Geoscience, Section 5.4 Hydrology, Potsdam, Germany 2 UN University, Institute for Environment and Human Security, Bonn, Germany
3 SIWRR Southern Institute of Water Resources Research, Ho Chi Minh City, Vietnam 4 Can Tho University, Mekong Delta Development Institute (MDI), Can Tho, Vietnam
Folie 2 Mekong Environmental Symposium | HCMC | 05-07 March 2013
Risk Definition
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Hazard- intensity- probability
Vulnerability- exposure
- susceptability
- coping capacity
- adaptation
Risk
Folie 3 Mekong Environmental Symposium | HCMC | 05-07 March 2013
Flood Hazard Analysis
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Current hazard
1. Flood frequency analysis for Kratie
2. For selected T generation of synthetic flood hydrographs
3. Hydraulic simulation of inundation of the Mekong Delta
Future hazard
1. Linking flood variability to monsoon variability
2. GCM scenarios for future monsoon variability
3. Estimation of future probabilities of floods
Folie 4 Mekong Environmental Symposium | HCMC | 05-07 March 2013
Flood Hazard Analysis
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Current hazard – flood frequency
• Bivariate: flood peak discharge (Q) and flood volume (V)
• Non-stationary: trends in flood regime of the Mekong
• Joint probability Q-V by copula Bivariate Q-V HQ100
Delgado et al. 2010
Folie 5 Mekong Environmental Symposium | HCMC | 05-07 March 2013
Flood Hazard Analysis
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Current hazard – hazard maps
• MC sampling of Q-V-pairs from copula
• Scaling of normalized characteristic flood hydrographs
• Hydraulic simulation of inundation
Folie 6 Mekong Environmental Symposium | HCMC | 05-07 March 2013
Flood Hazard Analysis
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Current hazard – hazard maps 2009
Median max inundation depth 95%-quantile map 5%-quantile map
Folie 7 Mekong Environmental Symposium | HCMC | 05-07 March 2013
Flood Hazard Analysis
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Future hazard – flood frequency 2050
• Exploiting the link of monsoon variability to flood variability non-stationary flood probability estimated by monsoon index
• Joint probability future Q-V by copula
• 14 GCMs, A1B emission scenario
• Sea level rise assumption MONRE: +34 cm in 2050
Folie 8 Mekong Environmental Symposium | HCMC | 05-07 March 2013
Flood Hazard Analysis
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Future hazard – hazard maps 2050 Median max depth Difference 2050 - 2009
Folie 12 Mekong Environmental Symposium | HCMC | 05-07 March 2013
Vietnam Risk Index: Concept and Architecture
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Folie 14 Mekong Environmental Symposium | HCMC | 05-07 March 2013
Indicators of the Vietnam Risk Index – Susceptibility
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Data sources: Population and Housing Census Household Living Standard Survey Statistical Yearbooks
Structure of Vietnam Risk Index
Folie 16 Mekong Environmental Symposium | HCMC | 05-07 March 2013
Conclusions
Integrative perspectives on hazard and vulnerability are essential to capture overall risk related to current and future flooding
Flood hazard in the Mekong Delta is determined by flood peak and volume need for joint probability assessment
Future flood hazard estimation is possible though climate-flood variability link GCM ensemble prediction of future hazard
Highest susceptibilities not (no longer) in the major flood zones. Are these already the effects of the ‚living with floods‘ policy since 2000?
Vulnerability index can be a helpful tool to capture hot spots of vulnerability and to guide the prioritisation of adaptation action and funding
Hazard modeling in combination with a dynamic element in vulnerability indices allows for the future development not only of hazard scenarios but of integrating risk scenarios focusing on risk pathways
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Folie 17 Mekong Environmental Symposium | HCMC | 05-07 March 2013
Thank you very much for your kind attention!
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