Droughts of the future – scenarios and prospects

Steven Wade and Jean-Philippe Vidal ... Worst UK rainfall droughts (Vidal and Wade, forthcoming) ... Possible changes in precipitation 3 winter months (OND). 0.
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Drought Ahead! February 27th, London

Droughts of the future – scenarios and prospects

Steven Wade and Jean-Philippe Vidal HR Wallingford

Acknowledgements •Effects of climate change on river flows and groundwater recharge – CL04 •Climate change and sewerage systems – CL10 •Defra Cross-Regional Research Programme •EA Severe Droughts project •Business Risks of climate change (SNIFFER) •EEA CC indicators •EC COP12 negotiations •EC-India CC research collaboration •HRW company research Page 2

Worst UK rainfall droughts (Vidal and Wade, forthcoming)

1971/2

1995/96 1995 1984

1921

1976 Page 3

Scenarios and prospects – too little or too much? •Future Scenarios • HadRM3/UKCIP02 • UKWIR/EA research • Changes to population & demand

•Prospects for rainfall drought •Prospects for changes in river flow and recharge •Prospects for water resources drought Page 4

Global warming (Forth Assessment Report, 2007)

Page 5

Global warming (Forth Assessment Report, 2007)

Page 6

Changes in precipitation patterns based on HadRM3 (Wade et al., 2006) 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

Control run 1961-1990 Page 7

1980

1990

2000

2010

Low Emissions

2020

2030

2040

Medium High Emissions

2050

2060

2070

2080

High Emissions

2090

2100

Changes in precipitation patterns based on HadRM3 (Wade et al., 2006) 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 Page 8

1990

2000

2010

Low Emissions

2020

2030

2040

Medium High Emissions

2050

2060

2070

2080

High Emissions

2090

2100

Jan

Feb

Mar

Changes in rainfall, 2020s

Apr

A2 scenario (UKWIR, 2007)

+ 22 % + 20 %

Mersey, NW England

+ 18 % 50

+ 16 %

40 30

-10 -20 -30

+8%

-40

rin Su g m m e Au r tu m n

in te r

Sp

De c De c

W

O ct N ov O ct N ov

g

p Se

Ju l

Au

ay

Ja n

Ju n

-50

+6%

M

+ 10 %

Ap r

Aug

b

Jul

0

ar

Jun

10

M

May

20

Fe

+ 12 %

Percent change

+ 14 %

+4%

Stour, SE England

+2% 40

0

30

Sep

Oct

Nov

Dec

-4 % -6 % -8 %

Percent change

20

-2 %

10 0 -10 -20 -30

-14 %

Page 9

UKWIR, 2007

rin Su g m m e Au r tu m n

in te r

W

-12 %

Sp

g

p Se

Ju l

Au

Ju n

ay M

Ap r

b

ar M

Fe

Ja n

-40

-10 %

The chance of a dry winter: Test & Itchen rainfall pdf 4.5

x 10

-3

1970s 2020s 2050s 2080s

4 3.5 3 2.5

04/05 & 05/06

2 1.5 1 0.5 0 Page 10

0

200

400

600 800 Precipitation (mm)

1000

1200

The chance of a dry winter: Test & Itchen cdf 1 1970s 2020s 2050s 2080s

0.9 0.8 0.7 0.6 0.5

Wetter winters

0.4 0.3 0.2 0.1 0 Page 11

Wetter 1 in 10 year dry winters No change in 1 in 40+ dry winters? 0

100

200

300

400 500 600 Precipitation (mm)

700

800

900

Future rainfall drought (Vidal and Wade, forthcoming) The number of three month extreme rainfall droughts (SPI3 indicator)

•‘Short’ rainfall droughts likely to increase three-fold

Page 12

Future rainfall drought (Vidal and Wade, forthcoming) The number of twelve month extreme rainfall droughts (SPI12 indicator)

•Little change in longer droughts •Reduction in 12 month rainfall droughts in the North, Scotland and Northern Ireland Page 13

Future rainfall drought (Vidal and Wade, forthcoming) The time spent in each drought class for the SPI3 indicator

Page 14

Future rainfall drought (Vidal and Wade, forthcoming) The time spent in each drought class for the SPI12 indicator

Page 15

Prospects for river flows – role of storage Multi-model, A2 scenario, 2020s (UKWIR, 2006) Tamar@Gunnislake (47001) 50 90% confidence intervals 50% confidence intervals median

40

Change in monthly flows (%)

30 20 10

BFI=46%

0 -10 -20 -30 -40 -50

J

F

M

A

M

J

J

A

S

O

N

D

Itchen@AllbrookHighbridge (42010) 50 90% confidence intervals 50% confidence intervals median

40

Change in monthly flows (%)

30 20 10

BFI=96%

0 -10 -20 -30 -40

Page 16

-50

J

F

M

A

M

J

J

A

S

O

N

D

Average changes in monthly flow for 70 catchments Multi-model, A2 scenario, 2020s (UKWIR, 2007)

Page 17

Page 18

1

29

00

04

04

00

00

8

9

1

2

1

(T 00 ha 3 m es 39 ) 01 6 39 02 0 39 03 7 40 01 1 42 01 410 0 1 (It 1 ch en 43 ) 00 5 47 00 9 48 00 4 52 01 6 53 00 9 54 01 6 54 04 G 0 R 2 ( G 3G R C 3 (3 Ms G ) C M s) AV ER AG E

39 00

28

27

27

26

14

Percent change in annual recharge

Prospects for recharge – little change but longer groundwater recession Multi-model, A2 scenario, 2020s (UKWIR, 2007)

15

10 Rainfall-runoff models GW models

5

0

-5

-10

-15

-20

-25

-30

-35

Entec

Prospects for water resources drought Water futures for the South East (Wade et al., 2006) 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 0.0

Page 19

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

WMLE

WMHE

NEMHE Scenario

GSLE

GSHE

0.0 WMLE

WMHE

NEMHE Scenario

GSLE

GSHE

Conclusions •The drought 2004/5 to 2006 was the result of several dry winters and low winter recharge •In a warmer climate winters will be wetter and summers drier - dry winters will still occur •Short droughts will increase three-fold (Aut/Sum/Spr) •River flows affected by change in seasonal climate and catchment characteristics – higher flows and recharge will be ‘squeezed’ into a shorter period – longer recessions •Water resources drought affected by WRZ characteristics (storage/licence), changes in demand and how we choose to adapt to climate change Page 20

Example project reports & research papers Vidal, J.P. and Wade, S.D. (2007). A framework for developing highresolution multi-model climate projections: 21st century scenarios for the UK. Int. J. Climatology (accepted). Vidal, J.P. and Wade, S.D. (2007). Multimodel projections of catchment-scale precipitation regime. J. Hydrology (submitted). Vidal, J.P. and Wade, S.D. (2007) Effects of climate change of river flows and groundwater recharge: Guidelines for resources assessments and UKWIR06 scenarios. UKWIR Report 05/CL/04/* Wade, S.D., Barnett, C. and Fenn, T. (2006). Climate change and water resources. Defra Cross-Regional Climate Change Impacts and Adaptation Research Programme: Topic C – Water. Wade, S.D., Jones, P.D. and Osborn, T. (2006). The impacts of climate change on severe droughts. Implications for decision making. Environment Agency Science Report: SC040068/SR3. Page 21