Water Resources and Climate Change

Jun 29, 2006 - DRIER SUMMERS. Page 22. Medway: Changes in monthly PET 2020s. Monthly PET factors. 0. 5. 10. 15. 20. 25. 30. 35. 40. Jan. Feb. Mar. Apr.
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Climate change - future droughts Kent Water Summit Thursday 29th June 2006 East Malling Conference Centre, Kent www.futuredrought.org.uk Steven Steven Wade, Wade, Jean-Philippe Jean-Philippe Vidal Vidal11 HR HR Wallingford Wallingford Acknowledgements: Acknowledgements: Defra Defra (Global (Global Atmospheres), Atmospheres), Environment Environment Agency, Agency, UKWIR, UKWIR, UKCIP, UKCIP, Project Project partners partners ~~ Met Met Office, Office, Lancaster Lancaster University, University, Entec Entec UK, UK, CRU, CRU, CEH, CEH, BGS, BGS, Anglian Anglian Water, Water, Southern Southern Water, Water, Veolia Veolia

HR Wallingford History 1947 1982

2005

Hydraulics Research Organisation is formed Privatisation to create Hydraulics Research Ltd New Froude Modelling Hall opened

Water

Floods

HR Wallingford Coasts

Maritime

Energy

Page 2

1

Outline Introduction\Background Global warming Modelling climate change Impacts on UK future drought:• Rainfall drought • Hydrological drought (River flows, reservoirs, groundwater levels) • Water resources

Conclusions Page 3

Global warming

2

Global warming: evidence Combined global land and marine surface temperature record from 1856 to 2004 (Source: Climate Research Unit, University of East Anglia).

Temperature change ºC

Page 5

1.0

Evidence: Warming can not be explained by ‘natural’ forcing factors observed

model simulation

0.5

0.0

-0.5 1850

1900

1950

2000

Page 6

3

Evidence: Warming can be explained when anthropogenic forcing included Temperature change ºC

1.0 observed

model simulation

0.5

0.0

-0.5 1850

1900

1950

2000

Page 7

Climate modelling

4

30km 2.5 lat

Global models e.g. The Hadley Centre third coupled model – HadCM3 Page 9

3.75 long

19 levels in atmosphere 1.25 1.25

20 levels in ocean HadleyCentre

-5km

Global temperature change (°C) to 2100

Page 10

5

The UK Climate Impacts Programme Climate change scenarios SUMMER

winter

UKCIP98 300km

UKCIP02 50km

BIC03 25km

UKCIPnext ??km

Page 11

Climate change in the South East Essex County Wide Action Plan (HR Wallingford, 2005)

Main projections for Essex by the 2080s: •Winter temperatures will increase by 2-3°°C •Summer temperatures will increase by 3-5°°C •Winter precipitation will increase by 13-25% •Summer precipitation will decrease by 24-47% •Average sea levels will increase by 26-86cm* •Extreme sea levels will increase by 80-140cm* *including regional isostatic subsidence as well as climate change Page 12

6

Impacts of climate change on Essex Precipitation change  Water resources  Flooding (inland) Temperature increase  Heat stress during summer  Risk to river/wetland ecologies  Heating of buildings  Cooling of buildings  Demand for water Page 13

Why should we be considering climate change? Climate change is happening and will impact on water There is high confidence in this fact. There is less confidence in the extent of change, But we can still plan for the potential consequences.

What can we do to limit the consequences? ADAPTATION – reducing impacts of climate change. MITIGATION – reducing future climate change.

Why do this if the projections are so uncertain? NO and LOW regret actions - benefits now. ‘Climate proof’ future infrastructure development

Principles for adaptation to climate change • Rigorous science + practical solutions + social engagement (Hunt, 2006) Page 14

7

Future Droughts Impacts of climate change on water resources

Background: Water Availability & Supply

CEE

SEE

Public Water Supply

Ground water

Surface Water

Anglian Water

50%

50%

Thames Water

25%

75%

Southern 80% Region

20%

Water Availability (Groundwater): (Environment Agency, 2001). Page 16

8

Background: Water Availability (Surface Water) Summer

Winter

(Environment Agency, 2001).

Page 17

The development & impacts of UK drought Climate change

Climate variability

High temperatures Increased evapotranspiration

DURATION

Reduced ‘effective’ rainfall Less runoff and recharge Increase soil moisture deficits Lower groundwater levels Reduced river flow Reduced habitat areas

Plant water stress Reduced biomass/yield Increased demand for water

‘Threatened’ or actual water supply shortage Drought Permits/Orders Page 18

Environmental Impacts

Social Impacts

Economic Impacts

DROUGHT Rainfall--Agricultural-- Hydrological-- Water Resources

Rainfall deficits (amount, timing, severity)

Socio-economic change

9

Potential impacts of climate change Rainfall drought

Change in monthly average rainfall 2020s _ River Medway Rainfall Factor Indicators

10 5

%

HadCM3 CGCM2 CSIRO-mk2 CCSR/NIES GFDL-R30 ECHAM4/OPYC3 Average of GCM factors

0 -5 -10 -15 -20 Average

Spreadsheet of 2020s monthly rainfall and PET factors for % all UK catchments (UKWIR/EA, 2006)

Page 20

Winter

Summer

Climate models

UKCIP02 LOW UKCIP02 MEDIUM UKCIP02 HIGH

15

PET Factor Indicators 25 20 15 10 5 0 Average

Winter

Summer

10

Medway: Changes in monthly rainfall 2020s Monthly rainfall factors Percent change from 1961-90

40

WETTER WINTERS

WETTER WINTERS

30 20 10 0 -10 -20 -30

DRIER SUMMERS

-40 Jan Feb Mar

Apr May Jun

Jul

Aug Sep Oct

Nov Dec

Page 21

Medway: Changes in monthly PET 2020s Monthly PET factors 40

MORE EVAPORATION

Percent change from 1961-90

35

MORE TRANSPIRATION

30

GREATER WATER LOSSES FROM PLANTS, SOIL and OPEN WATER

25 20 15 10 5 0 Jan

Feb

Mar

Apr

May

Jun

Jul

Aug

Sep

Oct

Nov

Dec

Page 22

11

Development of extreme scenarios based on climate models (HR Wallingford, 2005) Direct use of monthly RCM data to estimate changes in frequency of severe droughts (6 months & 2 year) Regional analysis of 9 grid squares Comparison of GCM outputs (6 models) to place RCM in context

NS ES

SS NI

NEE

NWE

CEE

SWE

SEE

Defra Cross-Regional Climate change programme

Page 23

Changes in precipitation patterns based on HadRM3 Defra Cross-Regional Climate South East of England change programme Possible changes in precipitation 3 summer months (JAS) 200

Total rainfall July-Aug-Sept (mm)

180 160 140 120 100 80 60 40 20 0 1960

1970

1980

Control run 1961-1990

1990

2000

2010

Low Emissions

2020

2030

2040

Medium High Emissions

2050

2060

2070

2080

2090

2100

High Emissions

Page 24

12

Changes in precipitation patterns based on HadRM3 South East of England Possible changes in precipitation 3 winter months (OND) 450

Total rainfall Oct-Nov-Dec (mm)

400 350 300 250 200 150 100 50 0 1960

1970

1980

Control run 1961-1990

1990

2000

2010

Low Emissions

2020

2030

2040

2050

2060

Medium High Emissions

2070

2080

2090

2100

High Emissions

Page 25

Defra Cross-Regional Climate change programme

Changing patterns of seasonal rainfall 2080s Medium High Emissions scenario compared to 1961-1990

Change in frequency of extreme dry conditions

East Scotland

South East England

1 in 20yr Dry Winter

23 yrs

18 yrs

1 in 10yr Dry Winter 1 in 20yr Dry Summer

12 yrs 9 yrs

10 yrs 7 yrs

1 in 10yr Dry Summer

5 yrs

4 yrs

Comments (--) No significant change

(x2) More dry summers

Page 26

13

0

0

2020s 2050s 2080s 2020s 2050s 2080s HadRM3 (A2) - Increase in1970s the frequency of ‘short’ rainfall ES SS droughts

1970s

25 Defra Cross-Regional Climate change programme 20 25

15

5 0

1970s

25 20

10 5 0

10

5

5

0

0

1970s

1970s

2020s 2050s NS

2020s 2050s 25 NEE

2080s

15

10

10

5

5 2020s 2050s NI

0

2080s

25

25

20

20

15

15

10

10

2080s

5

1970s

10 5

5 1970s

2020s 2050s ES

1970s

25 20

Page 27

15

2080s

15

2020s 2050s SWE 0

20

10

0

20

1970s

25

15

15

10

0

15

20

2020s 2050s CEE

0

1970s

2020s 2050s 25 NWE

2020s 2050s SS

2080s

2080s

20 15 10

20

5

1970s15 2020s 2050s NEE

1970s

2020s 2050s NWE

2080s

25 20

5

15

0 1970s

0

2080s

10

5

2080s

0

2080s

25

No. droughts in 30 yrs

10

20

25

HadCM3 HadRM3-a HadRM3--b HadRM3--c

20

15

25

Number of 6 months extreme droughts

10

1970s 2020s 2050s SWE

2020s 2050s 5 SEE 0 2080s

1970s

Time period

2080s 2020s 2050s SEE

2080s

HadRM3 (A2) - Increase in the frequency of ‘long’ rainfall droughts Defra Cross-Regional Climate change programme

Number of 24 months extreme droughts 5

5

4

4

3

3

2

2

2

1

1

1

0

0

5 HadCM3 HadRM3-a HadRM3--b HadRM3--c

4 3

Page 28

1970s

2020s 2050s NS

2080s

1970s

2020s 2050s ES

2080s

0

5

5

5

4

4

4

3

3

3

2

2

2

1

1

1

0

0

1970s

2020s 2050s NI

2080s

1970s

2020s 2050s NEE

2080s

0

5

5

5

4

4

4

3

3

3

2

2

2

1

1

1

0

0

1970s

2020s 2050s CEE

2080s

1970s

2020s 2050s SWE

2080s

0

1970s

2020s 2050s SS

2080s

1970s

2020s 2050s NWE

2080s

1970s

2020s 2050s SEE

2080s

14

Potential impacts of climate change River flows

Runoff factors based on UKCIP02 scenarios for the 2020s (UKWIR, 2003) Anglian 5

% change

0 -5

J

F

M

A

M

J

J

A

S

O

N

D

-10 -15 -20 -25 -30 low

medium

high

Southern & Wessex

Thames 10

10

J

F

M

A

M

J

J

A

S

O

-20 -30

N

D

% change

% change

0 -10

0 -10

low

medium

F

M

A

M

J

J

A

S

O

N

D

-30 -40 low

-40

J

-20

medium

high

high

Page 30

15

Change in river flows: 2020s UKWIR/EA CL-04 Medway@Teston (40003) 50 90% confidence intervals 50% confidence intervals median

40

Change in monthly flows (%)

30 20 10 0 -10 -20 -30 -40 -50 Page 31

J

F

M

A

M

J

J

A

S

O

N

D

Potential impacts of climate change Reservoirs

16

HadRM3H – perturbation to estimate source yields

Page 33

EA Severe Droughts Project

Potential impacts of climate change Groundwater

17

Change in recharge 2020s Itchen@AllbrookHighbridge (42010) 50 90% confidence intervals 50% confidence intervals median

40

Change in monthly recharge (%)

30 20 10 0 -10 -20 -30 -40 -50

J

F

M

A

M

J

J

A

S

O

N

D

Page 35

UKCIP02 Impacts on groundwater levels – Average changes in chalk in SE England (Bloomfield & Wade) 0.00 -0.20 -0.40 -0.60 -0.80 -1.00 Mean

-1.20

1 in 20 year

Point 3 ditto

08 0s H2

0s H

20 8

08 0s M

M

L2

H

20 5

0s

20 20 s H

0s 20 2 H M

M L2

L2 Page 36

02 0s

-1.40 02 0s

Change in groundwater level (metres)

Change in Minimum Groundwater Levels

Scenario

18

Water resources systems

Impacts of change on water resources Climate variability & Climate Change (UKCIP02 & HadRM3 Extremes)

Social & economic change (Foresight scenarios) •Population growth •Economic growth •Land use change •Social change •(Lifestyle & attitudes) Policy responses •Regulation •Investment •CAMS •WFD

Stakeholder responses •Business strategy •Risk “appetite” •Guidelines

 Temperature  Winter precipitation  Summer precipitation  PET  Variability

Environment

Responses

SUPPLY

DEMAND

Supply-demand balance •Risk •Uncertainty •(Headroom) •Least cost

Page 38

19

Water resources planning 260.00

Supply/Demand Ml/d

250.00

Planned schemes

Resources (no climate change)

Demand (climate and socio-economic change)

240.00 230.00 220.00

A

Increasing Deficit

D

19

25

B

210.00

Resources (with climate change)

200.00 190.00 1

3

5

7

9

11

13

15

17

21

23

Year

Demand

Page 39

Demand plus Headroom

Supply (Do Nothing)

Water futures for the SE: 2020s 80.0 Water Supply Agriculture Environment

Requirements Ml/d

70.0 60.0 50.0 40.0 30.0 20.0 10.0 0.0 Page 40

WMLE

WMHE

NEMHE GSLE Scenario

GSHE

Planned

20

Water futures for the South East 2020s Small increase in the demand (2%) for water due to climate change Large increases in demand for water in ‘growth areas’ due to increasing population/households Potential supply-demand deficits of 4 to 15% in the SE. Potential for additional investment ca. £50M per water resources zone in development ‘hot-spots.’

2050s Increase in demand (4%) due to climate change Increases in demand depending on socioeconomic scenario Potential supplydemand deficits of 7 to 32 % in SE

Water Futures: 2080s resource requirements =f(climate change, socio-economic change)

160.0

350.0

140.0

300.0

120.0 100.0 Water Supply Agriculture Environment

60.0 40.0

250.0 200.0 150.0 100.0 50.0

20.0

Page 41

Requirements Ml/d

Requirements Ml/d

Water Futures: 2050s resource requirements =f(climate change, socio-economic change)

80.0

2080s Further increases in demand due to climate change Overall increases depending on socio-economic scenario Potential supplydemand deficits of 16 to 46% in SE

0.0 WMLE

WMHE

NEMHE Scenario

GSLE

0.0

GSHE

WMLE

WMHE

NEMHE

GSLE

GSHE

Scenario

Management measures

Page 42

Supply

Demand

Environmental

National

National transfers (North to South) Research Monitoring of trends in rainfall, river flow and recharge

Educational projects Research into water saving technology Improved Building Regulations

Environmental Directives Implementation of the WFD New legislation on drought management

Regional

New reservoirs Reservoir raising Canal transfers Drought forecasting Conjunctive use Emergency planning

Tariffs for measured charges Restrictions to discretionary use

Negotiated environmental agreements Habitat corridors Regional Spatial Strategies

Local

Bankside storage Collective storage reservoirs Desalination Wastewater re-use Artificial recharge of aquifers Flexible licensing Insurance against crop failure

Waste minimisation Dual flush toilets Metering Leakage control Rainwater use Greywater use White goods subsidies Change crop types Improved irrigation technology

Abstraction controls & trading Emission controls Recreation and restoration of wetlands areas Rehabilitation projects

21

Multi-Criteria Analysis of Options Figure 3.3: Scatter Plot of Score versus Cost for the East of Scotland Case Study 100% 90% 80%

WW reuse (indirect pws)

WW reuse (direct pws)

Abstraction trading

WW reuse (direct non-pws)

70%

WW reuse (indirect non-pws)

Weighted Score

Educational projects Rainwater use

Tariffs

White goods subsidies

Retrofit of toilets

60%

Metering (domestic)

Pipeline transfer

Canal transfer

50%

Improved leakage control

40% Greywater use

30% Winter storage (farm consortium) Winter storage (single farm)

20%

Waste minimisation

Change crops

Change irrigation

10% 0% 1

10

100

1000

3

Cost (p/m )

Page 43

Conclusions: Climate change impacts •Three of the worst five rainfall droughts in the UK since 1914 have occurred since 1990 •‘Short’ droughts, lasting one or two seasons, will increase significantly by the 2050s and be commonplace by the 2080s •The chance of a ‘dry winter’ will remain unchanged •Pressures on public water supply, agriculture and the environment will increase •Public water supply-demand deficits of 4 to 15 % developed by the 2020s and deficits of 16 to 46 % by the 2080s for the baseline or ‘do nothing’ case. Page 44

22

Conclusions: Adaptation

Page 45

•improvements to drought risk management •variable water charges •changes to agricultural irrigation practices inc. small on-farm reservoirs • mandatory changes to land use planning and building regulations • as well as the ‘twin-track’ water resources planning approach of developing new resources alongside demand management schemes. •selecting adaptation measures to meet environmental, social and economic objectives (MCA)

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