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www.merseyforest.org.uk Green Infrastructure and Climate Change Dr Susannah Gill The Mersey Forest susannahgill@merseyforest.org.uk
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www.merseyforest.org.uk Overview Green infrastructure Climate change Green infrastructure for adaptation in urban areas Policy relevance in the UK North West Climate Change Action Plan Conclusions
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www.merseyforest.org.uk Green Infrastructure Life support system – the network of natural environmental components and green and blue spaces that lie within and between our cities, towns and villages and provide multiple social, economic and environmental benefits http://www.greeninfrastructurenw.org.uk
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www.merseyforest.org.uk Our Climate is Changing ( source : IPCC, 2007) Warming of the climate system is unequivocal Coherent changes in many aspects of the climate system not just temperature
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www.merseyforest.org.uk Changes go beyond natural variability Temperature change in last 50 years is very likely (>90% chance) due to increase in anthropogenic greenhouse gas concentrations (source: IPCC, 2007)
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www.merseyforest.org.uk Global climate change projections ( source : IPCC, 2007) (relative to 1980-99)
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www.merseyforest.org.uk What does this mean for the UK? UKCIP02 –4 emissions scenarios –3 time slices –50 km outputs (some 5 km) UKCIP08 –Probabilistic scenarios –25 km output –Due October 2008
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www.merseyforest.org.uk UK Climate Changes Average temp increases High temp extremes increase in frequency Low temp extremes decrease in frequency Sea-surface temp warms Thermal growing season lengthens Winter precipitation increases Winter precipitation intensity increases Greater contrast between summer & winter Snowfall decreases Summer soil moisture decreases Sea-level rises UKCIP02 High Confidence Levels
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www.merseyforest.org.uk Greater Manchester Average Maximum Summer Temperature Data from the UK Met Office and UKCIP02
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www.merseyforest.org.uk Greater Manchester Summer Precipitation Data from the UK Met Office and UKCIP02
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www.merseyforest.org.uk Greater Manchester Winter Precipitation Data from the UK Met Office and UKCIP02
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Baseline (1961-90) 2050s Low emissions 2050s High emissions 2080s High emissions Manchester (Mean Annual Temp) Slide courtesy of Mark Broadmeadow
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Baseline (1961-90) 2050s Low emissions 2050s High emissions 2080s High emissions Manchester (monthly mean temp, diurnal temp range & precipitation) Slide courtesy of Mark Broadmeadow
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Matt Cardy/Getty Images Source: The Guardian website Daniel Berehulak/Getty Images Kate Gillon/Getty Images
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Source: Stott et al, 2004 June-Aug temp anomalies (relative to 1961-1990 mean)
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www.merseyforest.org.uk Climate Change Management Smit et al (1999)
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www.merseyforest.org.uk Mitigation Role of GI Carbon sequestration & storage Direct fossil fuel substitution Material substitution Local food production Reducing need to travel
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www.merseyforest.org.uk Adaptation Role of GI Moderating temperature extremes Decreasing rate and volume of rainwater runoff Providing wildlife corridors Providing recreation spaces e.g. high capacity, less sensitive landscapes
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Key Stakeholders Town & Country Planning Association (Chair) Association of British Insurers Environment Agency North West Climate Group Office of the Deputy Prime Minister Royal Town Planning Institute South East Climate Group http://www.k4cc.org/Members/Claire/BKCC-Results-Publication.pdf
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ASCCUE Methodology Two case study areas –Greater Manchester –Lewes, Sussex Three exposure units –Integrity of the built environment –Human comfort –Urban greenspace Two case study areas –Greater Manchester –Lewes, Sussex Three exposure units –Integrity of the built environment –Human comfort –Urban greenspace
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Urban Greenspace Urbanisation alters –Micro-climate – increased temperatures –Hydrology – increased rate & volume of surface runoff Climate change alters temperature & rainfall patterns Urban greenspace can moderate ‘urban heat island’ effect and reduce rate & volume of runoff Therefore urban greenspace has potential to adapt cities to climate change Urbanisation alters –Micro-climate – increased temperatures –Hydrology – increased rate & volume of surface runoff Climate change alters temperature & rainfall patterns Urban greenspace can moderate ‘urban heat island’ effect and reduce rate & volume of runoff Therefore urban greenspace has potential to adapt cities to climate change
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Urban Morphology Types
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Urban Characterisation
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Greater Manchester Urban Morphology Types
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UMT Surface Cover
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‘Evapotranspiring’ Surfaces
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‘Urban’ Tree Cover
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Surface Cover and Residential Density
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Modelling environmental functions Use surface cover data as one input into surface temperature and runoff models Series of model runs –Current urban form Baseline and future climate –‘Development scenarios’ Baseline and future climate Use surface cover data as one input into surface temperature and runoff models Series of model runs –Current urban form Baseline and future climate –‘Development scenarios’ Baseline and future climate
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Maximum Surface Temperatures For a day occurring on average twice per summer
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Residential ± 10% green cover
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If grass does not evapotranspire… Maximum surface temperatures increase by –4.7-5.7°C in high density residential areas –13.8-15.6°C in schools Maximum surface temperatures increase by –4.7-5.7°C in high density residential areas –13.8-15.6°C in schools (Manchester Evening News, 2006)
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Occurrence of Drought for Grass Months/year when grass water stressed
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Adaptation in the Public Realm Surface temperature in tree shade here was 13°C cooler than in sun – large mature tree canopies provide more shade
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Surface Runoff 56% more rain results in 82% more runoff For a precipitation event occurring on average one day per winter, with normal antecedent moisture conditions
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Infiltration Capacity A case for ‘Conservation Areas’?
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Climatic adaptation via the green infrastructure Corridor Patch Matrix CorridorPatchMatrix Flood storage Infiltration capacity Evaporative cooling Shading Functional importance of urban greenspace needs to be reflected in plans, policies, strategies
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Summary of Findings Greenspace moderates temperatures through evaporative cooling & shading –Mature trees critical for shading Most effective in regulating surface runoff on high infiltration soils Increase rainwater storage Opportunity to use for irrigation in times of drought Greenspace moderates temperatures through evaporative cooling & shading –Mature trees critical for shading Most effective in regulating surface runoff on high infiltration soils Increase rainwater storage Opportunity to use for irrigation in times of drought
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Policy Implications Work across administrative boundaries & disciplines Protect critical environmental capital No net loss of green cover Creative greening Take opportunities in new development / restructuring Ensure water supply Work across administrative boundaries & disciplines Protect critical environmental capital No net loss of green cover Creative greening Take opportunities in new development / restructuring Ensure water supply
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www.merseyforest.org.uk Increasing Policy Relevance
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www.merseyforest.org.uk NW Climate Change Action Plan “Undertake scoping studies to assess future regional risks, opportunities and priorities for the potential for green infrastructure, including regional parks, to adapt and mitigate for climate change impacts and commence implementation of findings”
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www.merseyforest.org.uk GI functions for climate change MitigationAdaptation Biofuels production Timber production Food production Carbon storage Recreation Green travel routes Shading from sun Evaporative cooling Shading from sun Evaporative cooling Water storage Water interception Water infiltration Soil stabilisation Storm protection Habitat for wildlife Corridor for wildlife Recreation
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www.merseyforest.org.uk Conclusion Climate change mitigation role limited but important Climate change adaptation role substantial GI is a good adaptation strategy as it has other functions and benefits To maximise this need strategic planning at all levels, with functionality in mind Protect, create, enhance, and maintain
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