River Flood Damage Assessment using IKONOS images,
Segmentation Algorithms & Flood Simulation Models
Steven M. de Jong & Raymond Sluiter
Utrecht University
Corné van der Sande
Netherlands Earth Observation
Ad de Roo
JRC, European Commission, Italië
Department of Physical Geography – Utrecht University
Borgharen in January 1995
Two extremes 2002 versus 2003:
Full winter bed
&
Hardly room between the groynes
Department of Physical Geography – Utrecht University
10 years of flooding in NL
Is there an increasing trend?
Recurrence time of peak discharge
Borgharen 1993 & 1995 floods
Department of Physical Geography – Utrecht University
What to expect in the future...??
Analysis of
discharge over
the years:
- yearly peaks in black
- 15 yr average in red
- trend in blue
Joint JRC – UU project:
EC – JRC overall objectives:
1) Develop 'numerical' simulation tool for flooding in Europe: LISFLOOD
2) Apply it to larger catchments such as:
Rhine, Meuse, Oder, Severn, Elbe, Styre, Tisza, Gard
3) To evaluate the consequences of environmental measures:
buffer basins, afforestation, wider banks etc.
4) To increase flood forecast time
Our UU/JRC sub-objectives:
5) Quick assessment of damage, assessable in money, typically after
2 or 3 days after flooding on the basis of:
IKONOS satellite imagery, Dutch LGN cover maps & EU-CORINE
6) To refine hydraulic roughness maps (Manning) for LISFLOOD
Mmmh
Simulation of the 1995 Meuse Flood Event using LISFLOOD
for the floodplain of Borgharen
Requirements (transnational):
- Reliable rainfall data (temporal, spatial) in entire Meuse catchment
- Accurate DEM & channel characteristics
- Hydraulic roughness (Manning’s n)
- Initial (moisture) conditions
- Land use, land cover: CORINE, LGN3, Earth observation
- etc.
Department of Physical Geography – Utrecht University
Floodplain DEM
derived from
laser altimetry
Landsat TM 30* 30 m
6 may 2000
SPOT XS 20 * 20 m
6 July 1987
IKONOS 1 * 1 m
6 May 2000
Sources for land use & land cover (CORINE, LGN3)
Images available prior to launch IKONOS in 2001
Department of Physical Geography – Utrecht University
Animation of Borgharen flood (Meuse) in January 1995
• Improved hydraulic resistance estimate (Manning’s n)
• Direct damage assessment due to flooding
Reliable land cover maps are essential for:
1.
2.
Damage estimates based
Hydraulic resistance estimates
on land cover objects
based on look up tables of land cover
and water depth
Department of Physical Geography – Utrecht University
IKONOS image
Data acquisition:
6 May 2000; 10.31 hr
Spatial resolution:
1 meter pan-sharpened
Spectral bands:
Blue 450-530 nm
Red 520-610 nm
Green 640-720 nm
Near infrared 770-880 nm
at 11 Bits
Orbit around the earth:
682 km
sun-synchronous
Map projection
Full resolution IKONOS image Borgharen
Department of Physical Geography – Utrecht University
Topographic map 1:10.000
IKONOS derived 1:10.000
Buildings, in black derived from
Topographic map and from IKONOS image
TM_width Green Yellow Withering Vegetation Wavelength (nm) Ref lect ance -0.05 0.05 0.15 0.25 0.35 0.45 0.55 400 600 800 1000 1200 1400 1600 1800 2000 2200 2400 4 123 5 7
Traditional spectral-based supervised image classification
1
2
3
band 1
ba
nd 2
Department of Physical Geography – Utrecht University
Concept of Image Segmentation at Various Hierarchical Levels (eCognition)
Segmentation parameters
Homogeneity criterion IKONOS-2 bands used
Shape settings Segmentation
and classification level
Land use types
Blue Green Red NIR Scale
parameter Colour
parameter Shape parameter smoothness compactness Level 1 All yes yes yes yes 5 0.7 0.3 0.9 0.1 Level 2 Buildings no yes yes yes 10 0.5 0.5 0.9 0.1 Level 3 Roads no yes yes yes 30 0.5 0.5 0.9 0.1 Level 4 Agriculture, water,
large buildings and roads
no no yes yes 100 0.9 0.1 0.9 0.1
Segmentation approach and parameters of IKONOS image
Nearest neighbour classification through the various levels
e.g. forest at level 2; building at level 4
Results are very good
Main disadvantage:
algorithms are black box for the user
Department of Physical Geography – Utrecht University
IKONOS based land cover map
ground truth 111 112 113 114 115 141 143 132 151 211 212 221 241 331 41 43 50 sum users' accuracy class-map accuracy Residential building 111 18 0 0 3 0 3 0 0 0 0 2 0 0 0 0 0 0 26 0.69 0.44 Garden 112 0 10 0 0 0 0 0 0 0 0 0 0 0 1 0 0 0 11 0.91 0.56
Grass in built-up area 113 0 1 12 1 0 1 0 0 0 0 0 0 0 0 1 0 0 16 0.75 0.63 Pavement/other urban 114 4 1 0 39 0 1 0 1 7 0 0 0 1 2 2 0 0 58 0.67 0.57 Water side 115 0 0 0 0 1 0 0 0 0 0 0 0 1 0 0 0 0 2 0.50 0.25
Road 141 11 0 2 23 1 36 0 1 3 0 0 0 1 4 0 0 0 82 0.44 0.41
Railroad 143 0 0 0 0 0 0 4 0 0 0 0 0 0 0 0 0 0 4 1.00 1.00
Sand deposit area 132 0 0 0 0 0 0 0 7 0 0 0 0 0 0 0 0 0 7 1.00 0.50 Industrial company 151 0 0 0 10 0 0 0 5 17 0 0 0 0 0 0 0 0 32 0.53 0.40 Pasture 211 0 5 1 2 0 0 0 0 0 123 0 1 1 22 8 0 0 163 0.75 0.74 Winter wheat 212 0 0 0 0 0 0 0 0 0 1 37 0 0 0 0 0 0 38 0.97 0.80 Nursery 221 0 0 0 0 0 0 0 0 0 0 0 5 0 0 0 0 0 5 1.00 0.83 Fallow 241 0 0 0 0 0 0 0 0 0 1 0 0 42 0 0 0 0 43 0.98 0.89 Natural vegetation 331 0 0 0 0 0 0 0 0 0 0 3 0 0 4 0 0 0 7 0.57 0.10 Deciduous forest 41 0 0 0 0 1 0 0 0 0 2 3 0 0 3 23 1 0 33 0.70 0.52 Mixed forest 43 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 6 0 6 1.00 0.86 Water 50 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 32 32 1.00 1.00 IK ON OS c la ss ifi ca tio n sum 33 17 15 78 3 41 4 14 27 127 45 6 46 36 34 7 32 565 producers' accuracy 0.55 0.59 0.80 0.50 0.33 0.88 1.00 0.5 0.63 0.97 0.82 0.83 0.91 0.11 0.68 0.86 1.00 Overall accuracy 0.74 KHAT accuracy 0.70
Error matrix IKONOS classification Borgharen
n= 565 samples (field work, topo map, TM image, aerial photo)
image to be evaluated
reference / ground truth
Department of Physical Geography – Utrecht University
Data Sources for Estimating Manning’s n & Direct Damage:
Land Use Derived from
Manning derived from CORINE, LGN3, IKONOS
used in flooding
simulation model
Department of Physical Geography – Utrecht University
Borgharen flood extent maps derived from various sources
Flood event of January 1995
Model
simulations
Based on
ERS-1 Radar
Satellite
image
(Bristol
University)
Based on
Interpretation
of aerial photo
Department of Physical Geography – Utrecht University
Theory of flood damage assessment
(Vrisou van Eck, 2001; Kok, 2001 ; USACE, 1996; Penning-Roswell, 1994)
Direct damage:
loss of means, recovery damage
Indirect damage
business interruption, environmental damage, cleaning costs,
evacuation costs
Flood factors controlling damage:
water depth, velocity, duration, sediment concentration & size
wave/wind action, pollution load, water rise during flood onset
Economic & social variables
Infra structure properties
Warning time before flooding
Damage assessment functions proposed by Delft Hydraulics (WL)
S
the total damage [€]
α
i(h)
damage factor of damage category i, depending on water depth (h)
h
water depth (m)
n
id(h)
number of units in category i with flooding depth h [-],
S
imax
maximum damage per unit in category i [€],
m
number of categories [-].
Source:
Vis et al, Int Journal of River Basin Management vol.1 (1), pp.33-40
Department of Physical Geography – Utrecht University
Dam age functions
0.00 0.10 0.20 0.30 0.40 0.50 0.60 0.70 0.80 0.90 1.00 0.00 2.00 4.00 6.00 Water depth (m ) D a m a ge f a c
tor w inter w heat
roads industry residential building
US LOSS CURVES
Structure + Contents
0
20
40
60
80
-2.00
0.00
2.00
4.00
Inundation depth (m ) % d a ma g e SCS FIA USACE NHRC C/B=0.3International Models for flood damage assessment
SCS: Soil Conservation Service
FEMA: Federal Emergency Management Agency
USACE: US Army Corps of Engineers
NHRC: Natural Hazards Research Centre (Australia)
Department of Physical Geography – Utrecht University
Estimated flood (direct) damage maps
Estimated damage map for the 1995 flood of Borgharen
Dark red: high damage rates
Light red: low damage rates
White: no damage/no information
Total estimated
damage of 1995 event
€ 72.0 million
Department of Physical Geography – Utrecht University
Source: Kok et al., 2000, Risk of Flooding and Insurance in the Netherlands
Proc. The Second International Symposium on Flood Defence (ISFD 2002) Beijing, September 10-13, 2002
Damage estimate by insurance company (1 year after event)
Plans for flood mitigation:
-
wider river banks
- deeper river banks
- vegetation to slow down flow
- elevated dikes at locations
Department of Physical Geography – Utrecht University