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Real-time flood extent maps
based on social media
Arnejan van Loenen
Dirk Eilander
Patricia Trambauer
Jurjen Wagemaker (FloodTags.com)
Email: arnejan.vanloenen@deltares.nl
FloodControl 2015 – Dashboard Banjir Online
Pilot area: Jakarta
3
Frequent floods in
Jakarta
Feb 9th-11th 2015
• > 728 000 tweets
• peak 900 tweets/minute
• 2200 incl. water depth
• ~ 900 tweets (40%)
location
• For comparison: 10-20
water level gauges (not
all functioning)
“15.31 #Flood in Cipinang
Melayu where the water
level reaches up to +/ - 2m”
Flood observations in the “Twitter cloud”
Data integration platform: Delft-FEWS
Global Flood Monitor
5
Contents
• What social media can add to flood disaster management
• How to find the useful information
• Real-time flood mapping
• There is some uncertainty though
Information sources during floods
Telemetry CCTV
Rain radar Remote Sensing
Potential use of social media
8
-Finding flood prone areas
-validating hydrodynamic
models
- Currently flooded areas
- People in need
- Evacuation routes
Flood forecasting
Flood prevention
Disaster management
Disaster recovery - Flood Impact analysis
How to find the useful information
9
Is it a flood prone area?
Method 1: Height Above Nearest Drainage (HAND)
The HAND model normalizes topography according to the local
relative heights found along the drainage network
10
Is it a flood prone area?
Method 2: Slope
11
Is it a flood prone area?
12
• HAND (<3.5m) & Slope (<0.2 m-1) match well with flood
areas from MODISlance archive
• Uncertainty in threshold derived from bootstrapping HAND
and Slope flood areas
• Could be used to improve geo-location tweets
What is heavy rain?
13
90th percentile
99th percentile
Local hourly precipitationAccumulated daily precipitation
Contextual validation method
Static maps Dynamic maps
Weighted average taken as
Proxy for probability of flood
Real-time flood mapping
15
• Twitter Data
 5 Min resolution
 Water depth
 Location
• February 5th 2014
 Peak 250/5
minutes
Probabilistic approach
16
P = 0.3
P = 0.5
P = 0.2
x
x
x
Results 10 Feb 2015
17
York floods 2015: deterministic approach
29 m
0 m
0 5 102.5 Km
Generate flood plane
19
• Group observations by flowpath
• Interpolate water levels on reach
! Observation0 3 61.5 Km
29 m
0 m
0 5 102.5 Km
York floods, 2015
20
[1]
[3]
[5]
[2]
[6]
[9]
[11]
[10]
[8]
[7]
[4]
0 1 20.5 Km
Recorded Flood Extent
Mapped Water depth (m)
5 m 0 m
[4]
[1]
[3]
[5]
[2]
[6]
[9]
[11]
[10]
[8]
[7]
0 0.1 0.20.05 Km
Recorded Flood Extent
Mapped Water depth (m)
5 m 0 m
Uncertainty analysis
Uncertainty due to:
• Locational errors
• Elevation errors
• Water depth error
• Total uncertainty
21
[1] [2]
[3]
[4]
[5]
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! Validation Points
Mapped Water Depth
5 m 0 m
0 5 102.5 Km
Percentage Flooded
100% 50% 0%
0 5 102.5 Km
Percentage Flooded
100% 50% 0%
0 5 102.5 Km
Percentage Flooded
100% 50% 0%
0 5 102.5 Km
Percentage Flooded
100% 50% 0%
0 5 102.5 Km
Flood probability
Concluding
• There is a lot of useful information out there
• The information is real-time and (partly) publicly available
• The challenge is filtering out the useful data; real-time hydrological
data and tools can help
• Uncertainty in flood mapping due to location and observation error
• Quality of flood mapping increases by using hydrological
characteristics
• Useful flood maps can be generated using a low number of
observations
• Photos contain a lot of useful information
Questions?
Ideas for further development and possible
applications in projects are also welcome!
Arnejan.vanLoenen@deltares.com
+31(0)88335 8525
Dirk.Eilander@delteres.nl
+31(0)88335 7672

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DSD-INT 2016 Real-time flood extent maps based on social media - Van Loenen

  • 1. Real-time flood extent maps based on social media Arnejan van Loenen Dirk Eilander Patricia Trambauer Jurjen Wagemaker (FloodTags.com) Email: arnejan.vanloenen@deltares.nl
  • 2. FloodControl 2015 – Dashboard Banjir Online
  • 3. Pilot area: Jakarta 3 Frequent floods in Jakarta Feb 9th-11th 2015 • > 728 000 tweets • peak 900 tweets/minute • 2200 incl. water depth • ~ 900 tweets (40%) location • For comparison: 10-20 water level gauges (not all functioning) “15.31 #Flood in Cipinang Melayu where the water level reaches up to +/ - 2m”
  • 4. Flood observations in the “Twitter cloud” Data integration platform: Delft-FEWS
  • 6. Contents • What social media can add to flood disaster management • How to find the useful information • Real-time flood mapping • There is some uncertainty though
  • 7. Information sources during floods Telemetry CCTV Rain radar Remote Sensing
  • 8. Potential use of social media 8 -Finding flood prone areas -validating hydrodynamic models - Currently flooded areas - People in need - Evacuation routes Flood forecasting Flood prevention Disaster management Disaster recovery - Flood Impact analysis
  • 9. How to find the useful information 9
  • 10. Is it a flood prone area? Method 1: Height Above Nearest Drainage (HAND) The HAND model normalizes topography according to the local relative heights found along the drainage network 10
  • 11. Is it a flood prone area? Method 2: Slope 11
  • 12. Is it a flood prone area? 12 • HAND (<3.5m) & Slope (<0.2 m-1) match well with flood areas from MODISlance archive • Uncertainty in threshold derived from bootstrapping HAND and Slope flood areas • Could be used to improve geo-location tweets
  • 13. What is heavy rain? 13 90th percentile 99th percentile Local hourly precipitationAccumulated daily precipitation
  • 14. Contextual validation method Static maps Dynamic maps Weighted average taken as Proxy for probability of flood
  • 15. Real-time flood mapping 15 • Twitter Data  5 Min resolution  Water depth  Location • February 5th 2014  Peak 250/5 minutes
  • 16. Probabilistic approach 16 P = 0.3 P = 0.5 P = 0.2 x x x
  • 17. Results 10 Feb 2015 17
  • 18. York floods 2015: deterministic approach 29 m 0 m 0 5 102.5 Km
  • 19. Generate flood plane 19 • Group observations by flowpath • Interpolate water levels on reach ! Observation0 3 61.5 Km 29 m 0 m 0 5 102.5 Km
  • 20. York floods, 2015 20 [1] [3] [5] [2] [6] [9] [11] [10] [8] [7] [4] 0 1 20.5 Km Recorded Flood Extent Mapped Water depth (m) 5 m 0 m [4] [1] [3] [5] [2] [6] [9] [11] [10] [8] [7] 0 0.1 0.20.05 Km Recorded Flood Extent Mapped Water depth (m) 5 m 0 m
  • 21. Uncertainty analysis Uncertainty due to: • Locational errors • Elevation errors • Water depth error • Total uncertainty 21 [1] [2] [3] [4] [5] ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! !! ! ! ! ! ! ! ! ! ! ! ! !! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! Validation Points Mapped Water Depth 5 m 0 m 0 5 102.5 Km Percentage Flooded 100% 50% 0% 0 5 102.5 Km Percentage Flooded 100% 50% 0% 0 5 102.5 Km Percentage Flooded 100% 50% 0% 0 5 102.5 Km Percentage Flooded 100% 50% 0% 0 5 102.5 Km Flood probability
  • 22. Concluding • There is a lot of useful information out there • The information is real-time and (partly) publicly available • The challenge is filtering out the useful data; real-time hydrological data and tools can help • Uncertainty in flood mapping due to location and observation error • Quality of flood mapping increases by using hydrological characteristics • Useful flood maps can be generated using a low number of observations • Photos contain a lot of useful information
  • 23. Questions? Ideas for further development and possible applications in projects are also welcome! Arnejan.vanLoenen@deltares.com +31(0)88335 8525 Dirk.Eilander@delteres.nl +31(0)88335 7672