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31/03/2016
1
Adapting to climate change:
examples from the Netherlands
Workshop SDTA, ICID 26th ERC and 66th IEC, October 11-16, 2015, Montpellier, France
Henk Ritzema,
Wageningen University, The Netherlands
The Netherlands
Combination of
sea level rise
and subsidence
25% below sea level
65% would be flooded in
absence of dikes
31/03/2016
2
Agricultural development water management
In the past windmills
were used to drain
the land (left),
nowadays sluices
and barriers are used
to protect the land
against flooding
(right)
Water management
Land use
Climate change predictions:
Sea-level rise
Increase in river flow
Increase in winter precipitation
Higher risk of coastal flooding
Decrease in summer precipitation
Increase in temperatures
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3
Sea level rise and subsidence:
nothing new, but at a higher rate
Predicted sea level rise:
2100: 0.65 and 1.3 m
2200: 2 to 4 m
Predicted subsidence:
2100: 0.5 – 1.0 m
Pumping Dutch Polders to MSL -6m
- 5 m
0 m
+ 5m
Elevation in
m+ MSL
Den Haag
North Sea
Markermeer
A12
A4
A2Haarlem
A6
AmsterdamUtrecht
A13
A9A7
Waddenzee
Noordwijk
Delft
31/03/2016
4
- 5 m
0 m
+ 5m
Den Haag
North Sea
Markermeer
A12
A4
A2Haarlem
A6
AmsterdamUtrecht
A13
A9A7
Waddenzee
Noordwijk
Delft
Dutch Polder Landscape is inundated at MSL
Elevation in
m+ MSL
- 5 m
0 m
+ 5m
Den Haag
North Sea
Markermeer
A12
A4
A2Haarlem
A6
AmsterdamUtrecht
A13
A9A7
Waddenzee
Noordwijk
Delft
Pumping Dutch Polders to MSL -2m
Elevation in
m+ MSL
31/03/2016
5
- 5 m
0 m
+ 5m
Den Haag
North Sea
Markermeer
A12
A4
A2Haarlem
A6
AmsterdamUtrecht
A13
A9A7
Waddenzee
Noordwijk
Delft
Pumping Dutch Polders to MSL -4m
Elevation in
m+ MSL
Pumping Dutch Polders to MSL -6m
- 5 m
0 m
+ 5m
Den Haag
North Sea
Markermeer
A12
A4
A2Haarlem
A6
AmsterdamUtrecht
A13
A9A7
Waddenzee
Noordwijk
Delft
Elevation in
m+ MSL
31/03/2016
6
Climate change predictions:
Sea-level rise
Increase in river flow
Increase in winter precipitation
Higher risk of coastal flooding
Netherlands
=
‘sink’ of the Rhine Basin
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7
Peak discharge:Now: 16 000 m3/s
2100: 18 000 – 20 000m3/s
River Rhine: Peak discharge
15-25%increase
water level:
3m above MSL
↙ soil surface: 6m below MSL
Water head = 9 metres
Subsidence in combination with increased river flows
require higher river dikes
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8
Space for the river: creation of additional
storage capacity
River Rhine
Additional
storage
Flooding Risk in Dutch polder landscape
Flood-prone, heavily urbanised area, valuable in terms of‐ human settlements‐ industry‐ agriculture‐ ecology
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9
Increased risk of flooding/inundation
Risk-assessment maps on internet
For each province risk-assessment maps
can be consulted on the internet
Risk-
assessment
maps can be
consulted on
the internet
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10
Risk-assessment: public awareness
Public awareness is
difficult because risks
are small:
People do not follow-
up Government
instructions/advice
Climate change predictions:
Sea-level rise
Increase in river flow
Increase in winter precipitation
Higher risk of coastal flooding
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11
Change in rainfall: controlled Drainage
Rainfall:
↑ increase in winter
↓ decrease in summercontrolled
drainage
New paradigm: three step approach in drainage
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12
Controlled Drainage to reduce N Loading
Climate change predictions:
Sea-level rise
Increase in river flow
Increase in winter precipitation
Higher risk of coastal flooding
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13
Damage caused by flooding and subsidence
Flooding in residential areasRoads damaged by
uneven subsidence
Water mains and sewers damaged
by uneven subsidence
Smart solutions
Floating housesLiving with water
Floating greenhouses
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14
Consequences: development and O&M costs
will increase
0
50
100
150
200
(i) clay (ii) peat (iii) peat & water (iv) peat & sand
mill
ion e
uro
sInvestment costs O & M
Adaptation for 3 prevailing Soil Types:
ClaySandy soilsPeatLoam
3 Soil Types:• Peatlands• Reclaimed
clay soils• High sandy
4 Types of Land Use:
• Urban• Agriculture• Nature• Recreation
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15
Climate change: can we adopt ourselves?
Adapting to climate change: Examples from the Netherlands
Thank you for your attention
30