410 likes | 509 Views
TOUS CASE STUDY. MODELLER OVERVIEW REVIEW. COMPARATION AND ANALYSIS OF MODELLING RESULTS. 4th IMPACT WORKSHOP 3-5 NOVEMBER 2004. THE TOUS CASE STUDY. GENERAL VIEW. REMAINS OF THE TOUS DAM. THE CITY OF SUMACÁRCEL. THE TOUS CASE STUDY. AVAILABLE DATA.
E N D
TOUS CASE STUDY. MODELLER OVERVIEW REVIEW. COMPARATION AND ANALYSIS OF MODELLING RESULTS 4th IMPACT WORKSHOP 3-5 NOVEMBER 2004
THE TOUS CASE STUDY. GENERAL VIEW. REMAINS OF THE TOUS DAM THE CITY OF SUMACÁRCEL
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) CULTIVATED ZONES URBAN AREA SOIL EROSION SUMACÁRCEL DIFFERENCE BETWEEN BATHYMETRIES
THE TOUS CASE STUDY. FLOOD PROPAGATION GAUGE AND SECTION LOCATIONS.
THE TOUS CASE STUDY. SIMULATIONS. 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
THE TOUS CASE STUDY. CEMAGREF´S MODELLING. COARSE MESH FINE MESH
THE TOUS CASE STUDY. UCL´S MODELLING. REFINED MESH AROUND THE BUILDINGS
THE TOUS CASE STUDY. UDZ-1´S MODELLING. SIMPLIFIED CITY MODEL VIEW GENERAL VIEW OF THE MESH
THE TOUS CASE STUDY. UDZ-2´S MODELLING. GENERAL MESH VIEW CITY MODEL VIEW
URBAN FLOODING RESULTS. GAUGE 1. 1982 BATHYMETRY 1998 BATHYMETRY ~ 5000 s ≈ ~ 1h 15m • LOWER WATER LEVELS WITH 1982 BATHYMETRY • SLOWER CITY EMPTYING THAN EXPERIMENTAL • DIFFERENCES IN THE WAVE FRONT ARRIVAL GAUGE LOCATION PICTURE RIVER BED WAVE ARRIVAL VIEW
URBAN FLOODING RESULTS. GAUGE 2. 1982 BATHYMETRY 1998 BATHYMETRY • GOOD MAXIMUM RESULTS FOR BOTH BATHYMETRIES • DIFFERENCE IN THE WAVE SHAPE BETWEEN BATHYMETRIES • DIFFICULTIES DUE TO GAUGE 2 LOCATION GAUGE LOCATION PICTURE OLD CINEMA
URBAN FLOODING RESULTS. GAUGE 3. 1982 BATHYMETRY 1998 BATHYMETRY • MISTAKE IN THE GAUGE 3 LOCATION • UDZ-1 RESULTS WITH THE RIGHT LOCATION GAUGE LOCATION PICTURE CHURCH STREET
URBAN FLOODING RESULTS. GAUGE 4. 1982 BATHYMETRY 1998 BATHYMETRY • DIFFERENCE IN THE WAVE FRONT ARRIVAL TIME AND SHAPE BETWEEN BATHYMETRIES AND MODELLERS • UDZ-1 HIGHER LEVEL DUE TO AN UNKNOWN SET UP ERROR. GAUGE LOCATION PICTURE CONDES DE ORGAZ STREET
URBAN FLOODING RESULTS. GAUGE 5. 1982 BATHYMETRY 1998 BATHYMETRY • ~ 1m HIGHER WATER LEVELS • GAUGE 5 FOR 1998 BATHYMETRY LOCATED JUST OUT OF THE CITY MODEL FOR UDZ-1 JÚCAR STREET
URBAN FLOODING RESULTS. GAUGE 6. 1982 BATHYMETRY 1998 BATHYMETRY • ~ 1m HIGHER WATER LEVELS • SAME PROBLEM AS IN GAUGE 4 FOR UDZ-1 RESULTS • POTENCIAL RISK 2m WATER DEPTH AT SAME TIME GAUGE LOCATION PICTURE PROYECTO C STREET
URBAN FLOODING RESULTS. GAUGE 7. 1982 BATHYMETRY 1998 BATHYMETRY ~ 5000 s ≈ ~ 1h 15m • ~ 1m HIGHER WATER LEVELS FOR 1982 BATHYMETRY • WAVE ARRIVAL MORE ACCURATE IN 1998 BATHYMETRY • LOWER EMPTYING RATES THAN EXPERIMENTAL GAUGE LOCATION PICTURE OLD CITY HALL WAVE ARRIVAL VIEW
URBAN FLOODING RESULTS. GAUGE 8. 1982 BATHYMETRY 1998 BATHYMETRY LOWER FILLING UP RATES • ~ 1-2m HIGHER WATER LEVELS • LOWER FILLING UP RATES THAN EXPERIMENTAL GAUGE LOCATION PICTURE CLOCK´S SITE WAVE ARRIVAL VIEW
URBAN FLOODING RESULTS. GAUGE 9. 1982 BATHYMETRY 1998 BATHYMETRY • ~ 1m HIGHER WATER LEVELS WITH 1982 BATHYMETRY • GOOD RESULTS WITH 1998 BATHYMETRY GAUGE LOCATION PICTURE ERA SQUARE
URBAN FLOODING RESULTS. GAUGE 10. 1982 BATHYMETRY 1998 BATHYMETRY • ~ 2m DIFFERENCE WITH 1998 BATHYMETRY BETWEEN MODELLERS • ~ 1m DIFFERENCE WITH 1982 BATHYMETRY BETWEEN MODELLERS GAUGE LOCATION PICTURE JÚCAR STREET
URBAN FLOODING RESULTS. GAUGE 11. 1982 BATHYMETRY 1998 BATHYMETRY • ~ 2m HIGHER WATER LEVELS WITH 1982 BATHYMETRY • ~ 1.5m DIFFERENCE WITH 1998 BATHYMETRY BETWEEN MODELLERS GAUGE LOCATION PICTURE STAIRS STREET
URBAN FLOODING RESULTS. GAUGE 12. 1982 BATHYMETRY 1998 BATHYMETRY • SAME AND GOOD RESULTS FOR BOTH BATHYMETRIES GAUGE LOCATION PICTURE CONDES DE ORGAZ STREET
URBAN FLOODING RESULTS. GAUGE 13. 1982 BATHYMETRY 1998 BATHYMETRY • ~ 3m HIGHER WATER LEVELS WITH 1982 BATHYMETRY • GOOD RESULTS WITH 1998 BATHYMETRY • UDZ-2 LOWER WATER LEVELS DUE TO CITY MODEL GAUGE LOCATION PICTURE VALENCIA STREET
URBAN FLOODING RESULTS. GAUGE 14. 1982 BATHYMETRY 1998 BATHYMETRY • LOWER WATER LEVELS WITH 1982 BATHYMETRY • HIGHER WATER LEVELS WITH 1998 BATHYMETRY GAUGE LOCATION PICTURE PINTOR SOROLLA STREET
URBAN FLOODING RESULTS. GAUGE 15. 1982 BATHYMETRY 1998 BATHYMETRY • ~ 2m HIGHER WATER LEVELS WITH BOTH BATHYMETRIES GAUGE LOCATION PICTURE VALENCIA STREET
URBAN FLOODING RESULTS. GAUGE 16. 1982 BATHYMETRY 1998 BATHYMETRY • ~ 1.5m LOWER RESULTS WITH 1982 BATHYMETRY • GOOD RESULTS WITH 1998 BATHYMETRY GAUGE LOCATION PICTURE PINTOR SOROLLA STREET
URBAN FLOODING RESULTS. GAUGE 17. 1982 BATHYMETRY 1998 BATHYMETRY • ~ 2m HIGHER WATER LEVELS WITH 1982 BATHYMETRY • GOOD RESULTS WITH 1998 BATHYMETRY PALLECER STREET
URBAN FLOODING RESULTS. GAUGE 18. 1982 BATHYMETRY 1998 BATHYMETRY • GOOD RESULTS WITH 1982 BATHYMETRY • ~ 1.5m HIGHER WATER LEVELS WITH 1998 BATHYMETRY GAUGE LOCATION PICTURE SEVERO OCHOA STREET
URBAN FLOODING RESULTS. GAUGE 19. 1982 BATHYMETRY 1998 BATHYMETRY • SAME AND GOOD RESULTS WITH BOTH BATHYMETRIES FOR UCL AND UDZ-1 VIRGEN STREET
URBAN FLOODING RESULTS. GAUGE 20. 1982 BATHYMETRY 1998 BATHYMETRY • LOWER WATER LEVELS WITH 1982 BATHYMETRY • BETTER RESULTS WITH 1998 BATHYMETRY GAUGE LOCATION PICTURE VIRGEN STREET
URBAN FLOODING RESULTS. GAUGE 21. 1982 BATHYMETRY 1998 BATHYMETRY • GOOD RESULTS WITH BOTH BATHYMETRIES GAUGE LOCATION PICTURE WEST AVENUE
VALLEY FLOODING RESULTS. POINT A. 1982 BATHYMETRY 1998 BATHYMETRY ~ 3000 s ≈ ~ 50 m • SUBSTANCIAL DIFFERENCES IN WATER LEVELS BETWEEN MODELLERS • LOWER RESULTS WITH 1998 BATHYMETRY • DIFFERENCE IN THE WAVE FRONT ARRIVAL GAUGE LOCATION PICTURE 1 KM DOWNSTREAM TOUS DAM WAVE ARRIVAL VIEW
VALLEY FLOODING RESULTS. SECTION 1. 1982 BATHYMETRY 1998 BATHYMETRY • 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 GAUGE LOCATION PICTURE 1 KM DOWNSTREAM TOUS DAM
VALLEY FLOODING RESULTS. POINT B. 1982 BATHYMETRY 1998 BATHYMETRY • ~ 3m HIGHER WATER LEVELS WITH 1998 BATHYMETRY GAUGE LOCATION PICTURE AZUD
VALLEY FLOODING RESULTS. SECTION 2. 1982 BATHYMETRY 1998 BATHYMETRY • 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 GAUGE LOCATION PICTURE AZUD
VALLEY FLOODING RESULTS. POINT C. 1982 BATHYMETRY 1998 BATHYMETRY • SAME SHAPE OF THE WAVE FOR ALL THE MODELLERS WITH 1982 BATHYMETRY • HIGHER WATER LEVELS WITH 1998 BATHYMETRY GAUGE LOCATION PICTURE 3 KM DOWNSTREAM TOUS DAM
VALLEY FLOODING RESULTS. SECTION 3. 1982 BATHYMETRY 1998 BATHYMETRY • 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 GAUGE LOCATION PICTURE 3 KM DOWNSTREAM TOUS DAM
VALLEY FLOODING RESULTS. POINT D. 1982 BATHYMETRY 1998 BATHYMETRY - ~ 2m HIGHER WATER LEVELS WITH 1998 BATHYMETRY GAUGE LOCATION PICTURE BEFORE HILL UPSTREAM SUMACÁRCEL
VALLEY FLOODING RESULTS. POINT E. 1982 BATHYMETRY 1998 BATHYMETRY ~ 5000 s ≈ ~ 1 h 15 m • ~ 4m HIGHER WATER LEVELS WITH 1998 BATHYMETRY • SUBSTANCIAL DIFFERENCES IN THE WAVE FRONT ARRIVAL GAUGE LOCATION PICTURE RIVER BANK OPPOSITE SUMACÁRCEL WAVE ARRIVAL VIEW
VALLEY FLOODING RESULTS. POINT F. 1982 BATHYMETRY 1998 BATHYMETRY • ~ 3m HIGHER WATER LEVELS WITH 1998 BATHYMETRY • SUBSTANCIAL DIFFERENCES IN THE WAVE FRONT ARRIVAL • DOWNSTREAM BOUNDARY CONDITION EFFECTS GAUGE LOCATION PICTURE DOWNSTREAM SUMACÁRCEL
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