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High intensity! Future flood risk in urban and rapid response catchments Elliot Gill BSc FCIWEM C.WEM Global Practice Leader, Wet Weather & Wastewater Collection Co-authors: Murray Dale CH2M Elizabeth Kendon Met Office Hayley Fowler University of Newcastle Steven Chan University of Newcastle Barry Luck UKWIR Andrew Eden Environment Agency

High intensity! Future flood risk in urban and rapid ... · PDF fileconvective rainfall activity = more frequent flooding •Cities responsive to short duration ... Tool to convert

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High intensity!

Future flood risk in urban and rapid response catchments

Elliot Gill BSc FCIWEM C.WEM Global Practice Leader, Wet Weather & Wastewater Collection

Co-authors:

Murray Dale CH2MElizabeth Kendon Met OfficeHayley Fowler University of NewcastleSteven Chan University of NewcastleBarry Luck UKWIRAndrew Eden Environment Agency

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Agenda

• Our challenge

• The solution

• Preliminary climate change uplifts

• FCRM takeaways

• Related data outputs

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Our challenge

• Climate change predicted to increase storminess and local convective rainfall activity = more frequent flooding

• Cities responsive to short duration ( < 24hr ), intense and localised rain events

• Climate change guidance (Defra / EA) based on UKCP09 regional climate models (RCM)

• UKCP09 RCM @ 25km grid & not intended for sub-daily use

“water companies do not have a way of assessing the growing risk in sewer system management based on climate science”

“major gap in current industry knowledge”

United Kingdom Water Industry Research 2014

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The solution

• Use new Met Office high resolution climate models (1.5km grid)

• Single emission scenario 13 year simulation for 2100

• Derived spatial pattern of percentage uplift to current rain-event depths

– 2030, 2050 & 2080 epochs

– 3, 6, 12, 24 hr durations

– 10 and 30 year return period

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M30-601.5km grid 2100

100%

25%

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North West UK

North East UK

South UK

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Impact of storm duration & frequency

Uplifts are consistent across durations tested and between 10 year and 30 year return period

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UKWIR ‘central estimate’ uplifts to 30 year return period rainfall (<24 hr)

0

20

40

60

80

100

North West North East South Defra EA

%ag

e u

plif

t o

n c

urr

ent

clim

ate

2030s 2050s 2080s

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UKWIR ‘high estimate’ uplifts to 30 year return period rainfall (<24 hr)

0

20

40

60

80

100

North West North East South Defra EA

%ag

e u

plif

t o

n c

urr

ent

clim

ate

2030s 2050s 2080s

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Recommended uplifts

2030s 2050s 2080s

North West UK

Central estimate 20% 35% 55%

High estimate 35% 65% 110%

North East UK

Central estimate 10% 20% 35%

High estimate 30% 50% 85%

South UK

Central estimate 10% 15% 25%

High estimate 20% 35% 65%

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FCRM takeaways

1. Developed for use in urban drainage system & (pluvial) surface water appraisal & design.

2. Also applicable in rapid response fluvial catchments ?

3. Different to current EA guidance (esp. in North and all high estimates)

4. UKCP18 outputs will also use high resolution simulations but with added information on uncertainty

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30 % rainfall uplift = 40% to 130% flooding increase

60 % rainfall uplift =120 % to 280% flooding increase

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Timeseries (wet weather planning for combined sewer overflows)

Tool to convert historical timeseries into 2030s, 2050s, 2080s timeseries

Used in continuous simulation of sewer & river flows

Less drizzle, more larger storms, annual average similar

Thank You – Any Questions?

Visit stand B49…- Speak to me about my presentation- Find out more about CH2M- Play our interactive flood manager game and win…- Enjoy complimentary fresh fruit