Hydrologic forecasting for flood risk...
Transcript of Hydrologic forecasting for flood risk...
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Hydrologic forecasting for flood risk management
Predicting flows and inundation in data-limited catchments
Dr. Kelly KiblerAssistant professor
Civil, Environmental, & Construction EngineeringUniversity of Central Florida
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Roadmap1 Hydrologic forecasting for early warning
• Lead time• Accuracy• Challenge of the data-limited basin
2 Remotely sensed precipitation data • Opportunities and limitations• Designing observation networks to integrate remotely sensed
data3 Inundation
• Calibrating/validating hydrologic models
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Two critical components :1. Forecast accuracy 2. Forecast lead time
Flood Forecasting for Early Warning
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Two critical components :1. Forecast accuracy 2. Forecast lead time
Flood Forecasting for Early Warning
HOURS
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Two critical components :1. Forecast accuracy 2. Forecast lead time
Flood Forecasting for Early Warning
HOURS DAYS
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Two critical components :1. Forecast accuracy 2. Forecast lead time
Flood Forecasting for Early Warning
HOURS DAYS WEEKS
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Two critical components :1. Forecast accuracy 2. Forecast lead time
Flood Forecasting for Early Warning
HOURS
Increasing forecast lead time, increasing potential response and loss reduction
DAYS WEEKS
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Flood Forecasting for Early WarningEconomic benefit- damage/loss reduction
“In other words, for every USD 1 invested in this EWS, there is a return of USD 558.87 in benefits.” Subbiah and Bilden, 2008, World Bank Report
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Flood Forecasting for Early WarningEconomic benefit- damage/loss reduction: risk assessment in Surma River basin, Bangladesh
“Benefit-cost ratio of early warning system for a 5-year event was 2.71, 12.44 and 33.21 for 24 hours, 48 hours and 7 days lead time, respectively.” Hyder, 2013
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Important to accurately predict:1. Onset of flooding
flood stage
Flood Forecasting for Early Warning
Precipitation,
Discharge
time
Event
It started to rain.
Flooding
Peak of water level
Peak of rainfall
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Important to accurately predict:1. Onset of flooding2. Peak discharge
Precipitation,
Discharge
time
Event
It started to rain.
Flooding
Peak of water level
Peak of rainfall
flood stage
Flood Forecasting for Early Warning
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Important to accurately predict:1. Onset of flooding2. Peak discharge3. Duration of flood
Precipitation,
Discharge
time
Event
It started to rain.
Flooding
Peak of water level
Peak of rainfall
flood stage
Flood Forecasting for Early Warning
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Important to accurately predict:1. Onset of flooding2. Peak discharge3. Duration of flood4. Spatial extent of inundation, through time
Flood Forecasting for Early Warning
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Flood Forecasting for Early WarningTwo critical components :1. Forecast accuracy 2. Forecast lead time
Accuracy of forecast with 10 days lead time
Webster et al., 2010
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Flood forecasting in poorly gauged basins
Challenges:• Insufficient implementation and maintenance of ground-based,
real-time hydrologic observation.– Lag time between data observation and availability for flood forecasters.– Lead time compromised, poor forecasting skill.
• Management across boundaries.– Administrative barriers to data availability.
Manual data observation Basins cross boundaries Lack of transmission15
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Geopolitically ungauged catchment area
Geopolitically ungauged catchment area:Areas where comprehensive data observation networks may exist, but due to geopolitical constraints, catchments are effectively ungauged.
Hydrologic prediction in ungauged basins: a wicked problem for hydrologists
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Water-related disaster in transboundary river basins
Flood disasters in transboundary river basins:• Historically more severe, affect larger areas and result
in higher costs of human life and economic damages. • Suggests that international river basins may be
uniquely vulnerable to flood hazards.Bakker, 2009
Limitations in capacity for preparedness –a potential source of vulnerability in transboundary
basins? 17
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Integrated Flood Analysis System
Ground-gauged and/or satellite rainfall
Model creationRun-off analysis
River discharge, Water level, Rainfall distribution
Courtesy of JAXA
Global data: topography, land use, etc.
Aquifer modelRiver coursemodel
Surfacemodel
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• Several remotely-sensed precipitation products have global coverage. • Resolution (time and space) and observation accuracy are low
compared with ground observation rainfall.
SATELLITE RAINFALL IS NOT A SUBSTITUTE FOR AN OBSERVATION NETWORK!
Product name 3B42RT CMORPH QMORPH GSMaPBuilder NASA/GSFC NOAA/CPC NOAA/CPC JAXA/EORC
Coverage 50N~50S 60N~60S 60N~60S 60N~60SSpatial resolution 0.25° 0.073° 0.073° 0.1°Time resolution 3 hours 30 minutes 30 minutes 1 hour
Delay of delivery 6 hours 18 hours 3 hours 4 hoursCoordinate system WGS
Data archive Dec. 1997~ Recent 1week Recent 1week Dec.2007~
Data source(sensor)
Aqua/AMSR-E, AMSU-B,
DMSP/SSM/I and TRMM/TMI and IR
TRMM/TMI, Aqua/AMSR-E, AMSU-B, DMSP/SSM/I and IR
TRMM/TMI, Aqua/AMSR-E,
DMSP-F13-15/SSM/I, DMSP-F16-17/SSMIS,
IR data
IFAS – Satellite rainfall data
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present 1hour later 2 hours later
>
≒
3hour total
雨域の移動速度(停滞度)指標とピーク雨量比率の関係
Rain event with slow movement of rainy area
Rain event with quick movement of a rainy area
present 1hour later 2 hours later
3hour total
2
58 761 3 9
4
1 289
4
3 7
18923 5
6 7
56before
after
Yoshino river
Gro
und-
base
d / S
atel
lite
rain
fall
SlowquickMovement of rain area
correction methodto describe the difference of rainfall events
in terms of wind speed
Sate
llite
rain
fall
(GSM
aP) (
mm
/3h)
Ground rainfall (mm/3h)
IFAS – Satellite rainfall data calibration
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GSMaP(original) GSMaP(corrected)Ground gauged rainfall
3 hourly rainfall in Taiwan on typhoon Morakot, 2009 Aug.08 20-23(UTC)
• Corrected GSMaP is more accurate than raw data.
• User may specify any calibration equation.
IFAS – Satellite rainfall data calibration
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0
500
1,000
1,500
2,000
2,500
3,000
3,500
4,000
9/6 9/7 9/8 9/9 9/10Date (2004,GMT)
Dis
char
ge (m
3 /sec
)0
20
40
60
80
100
Rai
nfal
l (m
m/h
our)
Ground-gauged rainfallSatellite rainfall(3B42RT) 〃 (original GSMaP) 〃 (corrected GSMaP)Calculated discharge(Ground) 〃 (3B42RT) 〃 (original GSMaP) 〃 (corrected GSMaP)Measured discharge
SendaigawaRiver length =137km Basin Area =1,600km2 Correction of satellite data is successful
IFAS – Satellite rainfall data calibration
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0
500
1,000
1,500
2,000
2,500
7/4 7/5 7/6 7/7Date (2006,GMT)
Dis
char
ge (m
3 /sec
)0
20
40
60
80
100
Rai
nfal
l (m
m/h
our)
Ground-gauged rainfallSatellite rainfall(3B42RT) 〃 (original GSMaP) 〃 (corrected GSMaP)Calculated discharge(Ground) 〃 (3B42RT) 〃 (original GSMaP) 〃 (corrected GSMaP)Measured discharge
KikuchigawaRiver Length =71 km Basin Area =996 km2
IFAS – Satellite rainfall data calibration
Why was correction of satellite data unsuccessful?
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0
500
1000
1500
2000
2500
3000
3500
9/6 0:00 9/6 6:00 9/6 12:009/6 18:00 9/7 0:00 9/7 6:00 9/7 12:009/7 18:00 9/8 0:00
Date (UTC)
Dis
char
ge [
m3/s]
0
10
20
30
40
50
60
70
80
90
100
Rai
nfa
ll [m
m/h]
MWR observation
Ground gauged rainfall
GSMaP
Corrected GSMaP
Calculated discharge(GSMaP)Calculated discharge(Corrected GSMaP)Observed discharge
0
200
400
600
800
1000
1200
1400
1600
7/4 0:00 7/4 6:00 7/4 12:00 7/4 18:00 7/5 0:00 7/5 6:00 7/5 12:00 7/5 18:00 7/6 0:00
Date (UTC)
Dis
char
ge [m
3/s]
0
10
20
30
40
50
60
70
80
90
100
Rai
nfa
ll [m
m/h]
MWR observation
Ground gauged rainfall
GSMaP
Corrected GSMaP
Calculated discharge(GSMaP)Calculated discharge(Corrected GSMaP)Observed discharge
MWR observedfrequently
No MWR during peak rainfall
successful case : Sendai river unsuccessful case : Kikuchi river
Accuracy of rainfall area distribution depends on frequency of MWR observation
(& accuracy of IR motion vectors)
Image Source : JAXAOzawa et al. (2010)
IFAS – Satellite rainfall data calibration
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Forecasting Inundation for Early Warning
Bicol River basin, Philippines: simulated inundation extent and depth for a) 2-year, b) 5-year, c) 10-year, d) 25-year, e) 50-year and f) 100-year return periods.
d) 25 year
a) 2 year b) 5 year c) 10 year
e) 50 year f) 100 year
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The Rainfall-Runoff Inundation (RRI) model
Forecasting Inundation for Early Warning
Rainfall-Runoff Model
River Routing Model
Flood Inundation Model
• Rainfall-Runoff Model: simulating streamflow discharge with rainfall input.
• River Routing Model: tracking flood wave movement along an open channel with upstream hydrograph.
• Flood Inundation Model: simulating flooded water spreading on floodplains with inflow discharge.
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18Inundation map (2009-2010),
Pampanga river basin. Observed and simulated discharge
(2009-2010) at Arayat station.
Dis
char
ge (m
3 /h)
Traditional calibration with discharge
Dis
char
ge (m
3 /h) R
ainfall (mm
/h)
NSE=0.58
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Calibrating by spatial extent of inundation: RRI vs MODIS
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NDVI
22-30/09/2009“Ondoy”
8-16/10/2009“Pepeng”
8/10/2010-1/11/2010“Juan”
22-30/09/2009“Ondoy”
8-16/10/2009“Pepeng”
8/10/2010-1/11/2010“Juan”
NDFI1
22-30/09/2009“Ondoy”
8-16/10/2009“Pepeng”
8/10/2010-1/11/2010“Juan”
LSWI
22-30/09/2009“Ondoy”
8-16/10/2009“Pepeng”
8/10/2010-1/11/2010“Juan”
MLSWI
Comparison of inundation extent from RRI model and MODIS images using different NDSIs during selected flood events in Pampanga river basin. MODIS
RRI
0.3 0.29
0.140.30
0.25
0.100.25
0.24
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Sumary
1 Hydrologic forecasting for early warning• Objective to achieve long(er) lead time with confidence
(accuracy, or at least understanding of uncertainty) in data-limited basins.
2 Remotely sensed precipitation data • We still need ground-gauged precipitation, but do we need
the same information as before?3 Spatial inundation patterns
• Calibrating/validating hydrologic models using discharge or inundation through space and time?
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