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TOUS CASE STUDY. MODELLER OVERVIEW REVIEW. COMPARATION AND ANALYSIS OF MODELLING RESULTS 4th IMPACT WORKSHOP 3-5 NOVEMBER 2004
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THE TOUS CASE STUDY. GENERAL VIEW. REMAINS OF THE TOUS DAM THE CITY OF SUMACÁRCEL
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THE TOUS CASE STUDY. AVAILABLE DATA. - UPSTREAM BOUNDARY CONDITION → TOUS DAM OUTFLOW HYDROGRAPH - DOMWSTREAM BOUNDARY CONDITION → NOT FIXED - FRICTION PARAMETERS ● VALLEY FRICTION → MANNING 0.025 – 0.045 ● CULTIVATED ZONES FRICTION → MANNING 0.05 – 0.1 - BATHYMETRY 1982 / BATHYMETRY 1998 - CITY OF SUMACÁRCEL ● LOCATION OF THE BUILDINGS ● HEIGHT OF THE BUILDINGS - MAXIMUM WATER LEVELS AT SOME LOCATIONS (CITY AREA) SUMACÁRCEL CULTIVATED ZONES DIFFERENCE BETWEEN BATHYMETRIES SOIL EROSION URBAN AREA
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THE TOUS CASE STUDY. FLOOD PROPAGATION GAUGE AND SECTION LOCATIONS.
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THE TOUS CASE STUDY. URBAN FLOODING GAUGE LOCATIONS.
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THE TOUS CASE STUDY. SIMULATIONS. SIMULATION NUMBER OF CELLSCITY MODEL CEMAGREF COURSE MESH2611VERTICAL WALLS CEMAGREF FINE MESH~ 11000VERTICAL WALLS UCL R-760911VERTICAL WALLS UDZ-1~ 20000VERTICAL WALLS SIMULATION NUMBER OF CELLSCITY MODEL CEMAGREF COURSE MESH2611VERTICAL WALLS CEMAGREF FINE MESH~ 11000VERTICAL WALLS UCL R-560911VERTICAL WALLS UDZ-1~ 20000VERTICAL WALLS UDZ-2~ 40000BOTTOM ELEVATION 1982 BATHYMETRY 1998 BATHYMETRY REQUESTED RESULTS: - WATER DEPTH HISTORY AT GAUGE LOCATIONS - DISCHARGE HYDROGRAPH THROUGH SECTIONS - WATER DEPTH ENVELOPE OF 0.5 m AND 2 m
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THE TOUS CASE STUDY. CEMAGREF´S MODELLING. COARSE MESHFINE MESH
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THE TOUS CASE STUDY. UCL´S MODELLING. REFINED MESH AROUND THE BUILDINGS
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THE TOUS CASE STUDY. UDZ-1´S MODELLING. GENERAL VIEW OF THE MESH SIMPLIFIED CITY MODEL VIEW
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THE TOUS CASE STUDY. UDZ-2´S MODELLING. GENERAL MESH VIEW CITY MODEL VIEW
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- LOWER WATER LEVELS WITH 1982 BATHYMETRY - SLOWER CITY EMPTYING THAN EXPERIMENTAL - DIFFERENCES IN THE WAVE FRONT ARRIVAL URBAN FLOODING RESULTS. GAUGE 1. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE RIVER BED WAVE ARRIVAL VIEW ~ 5000 s ≈ ~ 1h 15m
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URBAN FLOODING RESULTS. GAUGE 2. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE OLD CINEMA - GOOD MAXIMUM RESULTS FOR BOTH BATHYMETRIES - DIFFERENCE IN THE WAVE SHAPE BETWEEN BATHYMETRIES - DIFFICULTIES DUE TO GAUGE 2 LOCATION
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URBAN FLOODING RESULTS. GAUGE 3. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE CHURCH STREET - MISTAKE IN THE GAUGE 3 LOCATION - UDZ-1 RESULTS WITH THE RIGHT LOCATION
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- DIFFERENCE IN THE WAVE FRONT ARRIVAL TIME AND SHAPE BETWEEN BATHYMETRIES AND MODELLERS - UDZ-1 HIGHER LEVEL DUE TO AN UNKNOWN SET UP ERROR. URBAN FLOODING RESULTS. GAUGE 4. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE CONDES DE ORGAZ STREET
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URBAN FLOODING RESULTS. GAUGE 5. 1998 BATHYMETRY1982 BATHYMETRY JÚCAR STREET - ~ 1m HIGHER WATER LEVELS - GAUGE 5 FOR 1998 BATHYMETRY LOCATED JUST OUT OF THE CITY MODEL FOR UDZ-1
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URBAN FLOODING RESULTS. GAUGE 6. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE PROYECTO C STREET - ~ 1m HIGHER WATER LEVELS - SAME PROBLEM AS IN GAUGE 4 FOR UDZ-1 RESULTS - POTENCIAL RISK 2m WATER DEPTH AT SAME TIME
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URBAN FLOODING RESULTS. GAUGE 7. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE OLD CITY HALL - ~ 1m HIGHER WATER LEVELS FOR 1982 BATHYMETRY - WAVE ARRIVAL MORE ACCURATE IN 1998 BATHYMETRY - LOWER EMPTYING RATES THAN EXPERIMENTAL WAVE ARRIVAL VIEW ~ 5000 s ≈ ~ 1h 15m
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URBAN FLOODING RESULTS. GAUGE 8. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE CLOCK´S SITE - ~ 1-2m HIGHER WATER LEVELS - LOWER FILLING UP RATES THAN EXPERIMENTAL WAVE ARRIVAL VIEW LOWER FILLING UP RATES
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URBAN FLOODING RESULTS. GAUGE 9. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE ERA SQUARE - ~ 1m HIGHER WATER LEVELS WITH 1982 BATHYMETRY - GOOD RESULTS WITH 1998 BATHYMETRY
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URBAN FLOODING RESULTS. GAUGE 10. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE JÚCAR STREET - ~ 2m DIFFERENCE WITH 1998 BATHYMETRY BETWEEN MODELLERS - ~ 1m DIFFERENCE WITH 1982 BATHYMETRY BETWEEN MODELLERS
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URBAN FLOODING RESULTS. GAUGE 11. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE STAIRS STREET - ~ 2m HIGHER WATER LEVELS WITH 1982 BATHYMETRY - ~ 1.5m DIFFERENCE WITH 1998 BATHYMETRY BETWEEN MODELLERS
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URBAN FLOODING RESULTS. GAUGE 12. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE CONDES DE ORGAZ STREET - SAME AND GOOD RESULTS FOR BOTH BATHYMETRIES
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URBAN FLOODING RESULTS. GAUGE 13. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE VALENCIA STREET - ~ 3m HIGHER WATER LEVELS WITH 1982 BATHYMETRY - GOOD RESULTS WITH 1998 BATHYMETRY - UDZ-2 LOWER WATER LEVELS DUE TO CITY MODEL
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URBAN FLOODING RESULTS. GAUGE 14. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE PINTOR SOROLLA STREET - LOWER WATER LEVELS WITH 1982 BATHYMETRY - HIGHER WATER LEVELS WITH 1998 BATHYMETRY
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URBAN FLOODING RESULTS. GAUGE 15. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE VALENCIA STREET - ~ 2m HIGHER WATER LEVELS WITH BOTH BATHYMETRIES
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URBAN FLOODING RESULTS. GAUGE 16. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE PINTOR SOROLLA STREET - ~ 1.5m LOWER RESULTS WITH 1982 BATHYMETRY - GOOD RESULTS WITH 1998 BATHYMETRY
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URBAN FLOODING RESULTS. GAUGE 17. 1998 BATHYMETRY1982 BATHYMETRY PALLECER STREET - ~ 2m HIGHER WATER LEVELS WITH 1982 BATHYMETRY - GOOD RESULTS WITH 1998 BATHYMETRY
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URBAN FLOODING RESULTS. GAUGE 18. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE SEVERO OCHOA STREET - GOOD RESULTS WITH 1982 BATHYMETRY - ~ 1.5m HIGHER WATER LEVELS WITH 1998 BATHYMETRY
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URBAN FLOODING RESULTS. GAUGE 19. 1998 BATHYMETRY1982 BATHYMETRY VIRGEN STREET - SAME AND GOOD RESULTS WITH BOTH BATHYMETRIES FOR UCL AND UDZ-1
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URBAN FLOODING RESULTS. GAUGE 20. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE VIRGEN STREET - LOWER WATER LEVELS WITH 1982 BATHYMETRY - BETTER RESULTS WITH 1998 BATHYMETRY
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URBAN FLOODING RESULTS. GAUGE 21. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE WEST AVENUE - GOOD RESULTS WITH BOTH BATHYMETRIES
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GAUGE LOCATION PICTURE 1 KM DOWNSTREAM TOUS DAM VALLEY FLOODING RESULTS. POINT A. 1998 BATHYMETRY1982 BATHYMETRY - SUBSTANCIAL DIFFERENCES IN WATER LEVELS BETWEEN MODELLERS - LOWER RESULTS WITH 1998 BATHYMETRY - DIFFERENCE IN THE WAVE FRONT ARRIVAL WAVE ARRIVAL VIEW ~ 3000 s ≈ ~ 50 m
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VALLEY FLOODING RESULTS. SECTION 1. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE 1 KM DOWNSTREAM TOUS DAM - SAME WATER FLOW RATE FOR BOTH BATHYMETRIES THROUGH SECTION 1 DESPITE THE DIFFERENCE IN WATER LEVEL - SAME PEAK AS IN THE OUTFLOW TOUS DAM HYDROGRAPH
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VALLEY FLOODING RESULTS. POINT B. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE AZUD - ~ 3m HIGHER WATER LEVELS WITH 1998 BATHYMETRY
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VALLEY FLOODING RESULTS. SECTION 2. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE AZUD - SAME WATER FLOW RATE FOR BOTH BATHYMETRIES THROUGH SECTION 2 DESPITE THE DIFFERENCE IN WATER LEVEL - SAME PEAK AS IN THE OUTFLOW TOUS DAM HYDROGRAPH
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VALLEY FLOODING RESULTS. POINT C. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE 3 KM DOWNSTREAM TOUS DAM - SAME SHAPE OF THE WAVE FOR ALL THE MODELLERS WITH 1982 BATHYMETRY - HIGHER WATER LEVELS WITH 1998 BATHYMETRY
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VALLEY FLOODING RESULTS. SECTION 3. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE 3 KM DOWNSTREAM TOUS DAM - SAME WATER FLOW RATE FOR BOTH BATHYMETRIES THROUGH SECTION 3 DESPITE THE DIFFERENCE IN WATER LEVEL - SAME PEAK AS IN THE OUTFLOW TOUS DAM HYDROGRAPH
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VALLEY FLOODING RESULTS. POINT D. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE BEFORE HILL UPSTREAM SUMACÁRCEL - ~ 2m HIGHER WATER LEVELS WITH 1998 BATHYMETRY
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VALLEY FLOODING RESULTS. POINT E. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE RIVER BANK OPPOSITE SUMACÁRCEL - ~ 4m HIGHER WATER LEVELS WITH 1998 BATHYMETRY - SUBSTANCIAL DIFFERENCES IN THE WAVE FRONT ARRIVAL WAVE ARRIVAL VIEW ~ 5000 s ≈ ~ 1 h 15 m
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VALLEY FLOODING RESULTS. POINT F. 1998 BATHYMETRY1982 BATHYMETRY GAUGE LOCATION PICTURE DOWNSTREAM SUMACÁRCEL - ~ 3m HIGHER WATER LEVELS WITH 1998 BATHYMETRY - SUBSTANCIAL DIFFERENCES IN THE WAVE FRONT ARRIVAL - DOWNSTREAM BOUNDARY CONDITION EFFECTS
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TOUS CASE STUDY. CONCLUSIONS. - COMPROMISE SOLUTION BETWEEN CELL SIZE AND TOPOGRAPHY CHARACTERISTICS - WATER LEVELS ADJUSTED TO THE TOUS OUTFLOW HIDROGRAPH OVER THE VALLEY - THE MOST “ECONOMICAL” CITY MODEL: VERTICAL WALLS ● MESHING DIFFICULTIES ● LONG DURATION OF SIMULATIONS - PROBLEMS WITH THE SELECTION OF DOWNSTREAM BOUNDARY CONDITION - MODELS SEEM TO REPRODUCE URBAN FLOODING SLOWER THAN IT WAS (FILLING UP AND CITY EMPTYING). - UNCERTAINTY IN THE RESULTS UP TO 5m IN THE VALLEY AND AROUND 2m IN THE URBAN AREA BETWEEN BATHYMETRIES AND MODELLERS
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