Management Plan 2026 - 2031
Climate
A changing climate, and adapting to its likely impacts, is the greatest challenge for the period of the Management Plan vision. The latest climate change projections for Somerset indicate warmer wetter winters, hotter drier summers with more extreme weather events such as heat waves, torrential storms coupled with rising sea levels. These changes will create significant impacts which will affect our landscapes, land use, communities, economy and infrastructures. Climate change and its impacts cut across all areas of this Management Plan, but this section provides a focus for principles, objectives and policies ensuring it is properly considered. ​
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5.1 Context and significance – Climate
Climate is dynamic and change has always occurred. However, over the last 150 years the level and scale of change have accelerated at an exponential rate. The levels of greenhouse gases in the atmosphere from human activities is trapping more heat causing warming at an unprecedented rate. It is one of the biggest challenges facing the world and is already causing irreversible damage to the planet and our way of life.
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The Intergovernmental Panel on Climate Change 6th Assessment Report shows that the average surface temperature in the UK has risen by 1.2oC since pre-industrial times and further warming is predicted even under all the decarbonisation pathways set out by the IPCC. The aim of limiting warming to 1.5oC looks increasingly difficult to achieve and risk assessment and adaptation plans are preparing for warming up to 4oC.
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UK climate projections suggest a change in rainfall patterns, and it is predicted that events now considered “extreme”, such as the exceptionally wet 2012 UK summer, will become more commonplace. It has been estimated that by 2035 an additional £20 million of spending on flood defences annually will be needed to maintain current levels of flood risk. Adaptability to climate change is a key consideration for future flood and coastal erosion management plans. However, the Committee on Climate Change has recently warned of national underinvestment in long term adaptive flood management.
There are predictions for climate change impacts on the natural environment – if hotter, drier summers and warmer, wetter winters materialise some species may disappear from the Quantock Hills and others may start to colonise including new pests and diseases. Timings of biological events may also alter: hatching times for some moth species are already thought to be changing in the National Landscape, affecting the breeding success of pied flycatchers and other migrant species in the upland oakwoods.
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Frequent summer droughts and an increase in wildfires may lead to significant species change in our heathland and the upland oakwoods could be subject to increased storm damage and disease. The risk of flooding of all types may be increasing with potential landscape-specific impacts such as rising sea levels affecting coastal and intertidal habitats, while storm surges could lead to an increased level of coastal erosion.
Arable farming may increase with farmers able to grow new crops or varieties and extend the growing period for current ones, however farming is likely to become more challenging with greater extremes of temperature and rainfall and more frequent damaging storms.
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Water resources are likely to be stretched with more severe drought periods, perhaps leading to pressure for new reservoir storage capacity in upland catchments. Drought will also have implications for the management of hill livestock, with limited natural watering places.
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Climate change is, in part, driven by human activity including land use. Appropriate land use and actions that can capture carbon, known as sequestering, can be achieved through small measures and have additional benefits for biodiversity. Further nature-based solutions, as well as sequestering carbon, have other benefits in terms of climate such as reducing flood risk. Regenerative agricultural systems can improve soil health, increasing resilience of grasslands and crops to climate extremes. Enhancement of soil structures and management will enhance carbon storage, called carbon stocks, within those soils. Some habitats in the Quantock Hills, such as unimproved grasslands and upland heathlands already have high carbon stocks. Therefore, the likely carbon stock of existing habitats should be taken into account when planning habitat change ensuring carbon stores are not lost. Restoring habitats such as unimproved grasslands or creating woodlands in the right location will increase carbon sequestration across the Quantock Hills, as well as providing other benefits such as nature recovery or flood risk mitigation.
Land management is not the only source of carbon emissions within the Quantock Hills. Other sectors such as energy use, transport, the built environment, business and water resources all have the potential to generate carbon emissions. The need to move away from a fossil-fuel based economy is essential, however it needs to be coupled with a reduction in resource demand, using less energy, reducing waste and encouraging greater efficiency.
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The rural landscape of the Quantock Hills can make it harder to make the transition to zero carbon. Some climate change mitigation and adaptation measures have the potential to adversely affect the natural beauty of the National Landscape, but with careful design and implementation, measures can conserve and even enhance the special qualities of the Quantock Hills. However, it is a significant challenge to develop a pathway to net zero which also conserves and enhances the natural beauty.
Mitigation and adaption
Climate change mitigation are actions that reduce or prevent greenhouse gases emissions from human activities. Slowing down the increase in greenhouse gases will slow the pace of climate change reducing the worst consequences.
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From the UNDP – What is climate change? reducing greenhouse gas emissions can be achieved by:
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Reducing use of fossil fuels. Fossils fuels are the biggest sources of greenhouse gas emissions and transitioning to renewable energy sources such as solar, wind and geothermal power and developing sustainable modes of transportation is crucial.
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Improving energy efficiency. Using less energy overall, in buildings, industries, public and private spaces, energy generation and transmission, and transportation will reduce emissions. This can be achieved through changes such as better insultation in buildings, increasing energy efficiency in appliances and improving energy transmission systems.
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Changing agricultural practices. Certain farming methods release high amounts of methane and nitrous oxide, which are potential greenhouse gases. Regenerative agricultural systems – including improving soil health, reducing livestock-related emissions, direct seeding techniques and using cover crops – support mitigation, improve resilience and decrease costs for farmers.
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Sustainable management and conservation of forests. Woodlands act as carbon sinks, absorbing carbon dioxide and reducing the overall concentration of greenhouse gases in the atmosphere. Measures to reduce deforestation and forest degradation are key for climate mitigation and generate multiple additional benefits such as biodiversity conservation and improved water cycles.
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Restoring and conserving critical ecosystems. In addition to forests, habitats such as wetlands, peatlands and grasslands also contribute significantly to carbon sequestration, while supporting biodiversity and enhancing climate resilience.
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Creating a supportive environment. Investments, policies and regulations that encourage emission reductions, such as incentives, carbon pricing and limits on emissions from key sectors are crucial to driving climate change mitigation.
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Somerset's Climate Emergency Strategy identifies that the climate will move towards warmer wetter winters, increased severity of storms and hotter, drier summers. These changes to our climate are already impacting our landscape affecting the special qualities of the Quantock Hills.
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Climate change adaptation refers to actions taken to adjust to a warming world and the likely weather patterns expected. The Quantock Hills National Landscape can play a vital role in adapting to climate change and building resilient landscapes for future generations.
Since 2015 the Quantock Hills National Landscape Partnership has worked in partnership with FWAG-SW, Natural England and others promoting natural flood management (NFM) strategies in the Quantock Hills. Natural flood management harnesses the natural processes of rivers, floodplains and coastlines to reduce flooding and coastal erosion. In practice these can take the form of woody dams, blocking drainage channels, rewetting peat bogs, creating or restoring ephemeral ponds, which allow land to hold water longer and sustain river flow during dry periods. The typography of the Quantock Hills, with a significant number of very small stream systems feeding into a number of water catchments and steep headwaters provides opportunities for nature-based solutions. To make meaningful contributions to there will need to be significant numbers of these. As part of this a four-year project was undertaken which installed woody dams and “ghost” ponds at a number of locations across the hilltops as part of FWAG-SW Hills to Levels project, funded by the Somerset Rivers Authority (SRA). This showed the benefit of nature-based solutions and highlighted the need for further work and research into the most effective use of this type of strategies.
Taking a risk assessment approach provides an opportunity to identify climate risks, incorporate them into management processes and encourage early engagement with stakeholders to address climate change challenges.
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The Quantock Hills National Landscape Partnership undertook a climate change risk assessment in 2024 – see appendix 2 [pdf] for the full risk assessment – which highlighted the following risks: ​
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Geology
Headline projection​​​
Sea level rise 0.27 – 1.13m by 2100
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Wetter winters
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Projected impact
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Increase in erosion of coastal area (D).
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Increased sustained coastal flooding (low lying land) (D). ​
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Increased coastal flooding.
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Altered flow regimes / greater fluctuation of water tables.
Risk and opportunity
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Risk of loss of geological interest, coastal agricultural fringe.
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Increased salination of coastal agricultural fringing land.
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Risk of flooding.
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Changes in plant communities favouring wetland plant communities.
Sessile oakwoods
Headline projection​​​
Increased mean temperatures, leading to longer growing season and altered phenology
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Warmer wetter winters
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Summer droughts more common and intense
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Increased extreme weather events – high winds
Projected impact
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Decline in bryophyte / moss species.
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Breakdown in synchrony between species due to changes in time of flushing.
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Increased shading due to increased and earlier canopy.
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Increased threat from pests / diseases.
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Expansion of existing pests / diseases e.g. P. ramorum responsible for oak dieback.
Improved winter survival of mammal pests such as deer and squirrel.
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Reduced soil moisture and drought.
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Increased risk of wildfire.
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Increased wind throw.
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Risk and opportunity
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Loss of bryophyte / moss species and associated invertebrate assemblages.
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Decline in key species and breakdown in food web.
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Changed in ground flora composition and regeneration.
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​Risk of loss of habitat.
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Risk of loss of habitat / species.
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Reduced regeneration and loss of ground flora.
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Decline and potential loss of sensitive ground flora.
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Fire could result in localised changes to ground flora and understorey composition.
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Risk of rowan / birch dominance.
Mixed ash-dominated woods
Headline projection​​​
Warmer wetter winters.
Summer droughts more common and intense.
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Increased extreme weather events – high winds.
Projected impact
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Expansion of existing pests / diseases e.g. P. ramorum responsible for oak dieback.
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Improved winter survival of mammal pests such as deer and squirrel.
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Reduced soil moisture and drought.
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Increased risk of wildfire.
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Increased wind throw.
Risk and opportunity
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Risk of loss of habitat / species.
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Reduced regeneration and loss of ground flora.
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Decline and potential loss of sensitive ground flora.
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Fire could result in localised changes to ground flora and understorey composition.
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Risk of rowan / birch dominance.
Heathland
Headline projection​​​
Warmer wetter winters.
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Increased mean temperatures.
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Hotter, drier summers.
Projected impact
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Reduced management options through burning or cutting (earlier bird breeding).
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Increased surface runoff.
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Increased nitrogen deposits.
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Longer growing seasons.
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Increased evaporation / drought.
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Increased risk of wildfire.
Risk and opportunity
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Risk of scrub encroachment.
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Opportunity for bilberry.
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Opportunity for Dartford warbler.
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Loss of habitat or waterlogging.
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Loss of nutrient-poor species.
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Increased sensitivity of heather to drought, frost and heather beetle.
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Dwarf shrubs become less dominant.
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Drying out and oxidation of peat soils change species composition and reduce carbon store / sequestration.
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Surface soils / peat drying out and increase wind blow (erosion).
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Loss of habitat structural diversity, potential local scale species extinction, especially for wet heath species.
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Increased frequency and intensity of fire could lead to species change favouring grass species.
Acidic / neutral dry grasslands
Headline projection​​​
Wetter and warmer winters.
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Drier summers.
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Hotter summers.
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Economics.
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Projected impact
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Soil erosion, compaction of soil (reduced incidents of frost heave).​​​
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Change in composition to favour annual over perennial species.
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Reduction in grass production.
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Drier conditions favour deep rooted plant species.
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Increased risk of wildfire.
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Longer growing season.
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Reduced livestock grazing.
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Risk and opportunity
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Risk to soil health, risk of soil erosion.
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Risk to soil health, risk to grazing and livestock.
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Risk to grazing livestock and species diversity.
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Risk to natural carbon stores and sequestration.
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Change in composition of grassland leading to increased bare ground and invasive species.
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Change in composition of grassland due to earlier flowing and seeding.
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​Increased spread of invasive species such as bracken.
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Reduced grazing stock / intensified grazing systems / conversion to arable production.
Beech hedgebanks
Headline projection​​​
Summer droughts more common and intense.​​​
Warmer summers.​​
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Increased frequency of extreme weather.​
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Warmer winters.​​
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Projected impact
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Suppression of growth, increased prevalence of drought stress
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Increase frequency and duration of high temperature incidents.
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High winds
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Higher intensity rainfall events leading to peak flows increasing by 40% by 2080.​​
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Reduced late frost events.​
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Risk and opportunity
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Reduced growth and spread of beech.
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Increased sun scorch leading to bark death in beech.
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Increase loss of trees and banks to wind throw
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Reduced nutrient uptake and reduce vigour of beech trees.
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Increased survival of pest species (squirrel, deer etc) result in more damage to trees.
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More generations of insect pests per year.
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Reduced bud initiation.
Native hedgerows
Headline projection​​​
Increased frequency of extreme weather.
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Increase in average temperature.
Warmer winters.
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Drier summers.
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Economics.​​​​
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Projected impact
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Higher intensity rainfall events leading to peak flows increasing by 40% by 2080.
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High winds.
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Longer growing season.
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Fewer frost events.
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Drought.
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Changing agricultural systems.
Risk and opportunity
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Increased flooding and soil saturation – damage to soil structures, difficulty in winter management.
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​Increase loss of mature and veteran trees.
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Increased growth and vigour of hedgerows.
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Reduced bud, flower and fruit production impacting wildlife.
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Increased die back of some species and increased stress increasing susceptibility to pests and diseases
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Intensification of adjacent land use leading to impacts such as pesticide drift and nutrient enrichment.
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Intensification leading to reduction of buffer strips and margins increasing damage and impact on hedges.
Traditional orchards
Headline projection​​​
Warmer drier summers.
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Warmer wetter winters.
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Increased frequency of extreme weather.​​​​​​​​​​​​​​​​
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Projected impact
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Drought.
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Warmer temperatures with longer growing season.
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Fewer frost events.
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​Higher intensity rainfall events leading to peak flows increasing by 40% by 2080.
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High winds.
Risk and opportunity
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Increase root stress, reduction in fruit production.
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Increased and new pest damage.
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Increase of disease such as powdery mildew and fire blight.
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Traditional orchard fruit species replaced by fruit currently grown in more southerly locations. Impact on insect species dependant on current fruit species.
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Greater survival of insect pests with higher populations and impact on trees.
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Inadequate periods of complete dormancy risking trees flowering early, at different times from pollinators or development of blind buds.
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Increase in diseases such as scab (warmer, wetter winter) and phytophthora spp (waterlogged soils).
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Prolonged wet soil conditions increase risk of tree death from water logging.
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Increased wind throw especially of mature trees.
Climate change adaptation plans
The Government’s 2023 Climate Adaptation Strategy under the Third National Adaptation Programme (NAP3) requires all Protected Landscapes to produce climate change adaptation plans, embedded in or linked with their management plans by 2028. The Quantock Hills Climate Change Risk Assessment (appendix 2 [pdf]) is the first step in producing the adaptation plan with actions in year 1 and 2 to identify policy responses, relevant local stakeholders and work together to set out planned actions for the short, medium and long term.
Headline projection​​​
Increased frequency of extreme weather.
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Projected impact
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Increase in frequency and severity of high rainfall events.
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​Increase in frequency and severity of high wind events.
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Risk and opportunity
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Locally distinct heritage (properties) at increased risk of flooding.
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Locally distinct heritage at increased risk of damage due to high intensity rain / wind events e.g. structural damage to roof.
Built environment – locally distinctive buildings in Quantock Hills villages
5.2 Guiding principles - Climate
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Principle 1: The climate and nature crises are intrinsically linked
Climate change is in part driven by human land use, and in turn, a changing climate is exacerbating loss of biodiversity across the Quantock Hills as elsewhere. However, actions that help reverse biodiversity loss will also contribute to increasing carbon sequestration and help make the landscape more resilient to climate instability.
Principle 2: The way we manage the land will have a huge effect on how well we can cope with a changing climate
Nature-based solutions have an important role to play in tackling climate change, e.g. by reducing flood risk in the river catchments impacts by the Quantock Hills, while also improving conditions and habitats for wildlife. Meanwhile regenerative approaches to farmland management improve the resilience of soils and crops to climate extremes.
Principle 3: Soils and vegetation store a lot of carbon, and some store more than others
Some habitats in the Quantock Hills like heaths and woodlands, already have high carbon stocks. Therefore, carbon content should be borne in mind when prioritising habitat creation or restoration, and trade-offs between habitats need to take account of carbon implications.
Principle 4: We can store a large amount more carbon in our landscape
Restoring habitats like permanent grassland and creating new woodlands in the right locations across the Quantock Hills, will increase carbon sequestration as well as helping wildlife. And across the whole Quantock Hills farmed landscape, modest changes in land management practices could have a large cumulative effect on carbon storage.
Principle 5: We need to work urgently to mitigate climate change, as well as taking measures to adapt to it
There is a role for all those working in the Quantock Hills to promote and implement lower carbon lifestyles, through organisations’ own activities to minimise their carbon footprint, and by promoting local food, choosing venues accessible by public transport, online meetings, etc.
Principle 6: We need to minimise energy consumption wherever possible
Our collective response to the climate crisis is unlikely to succeed if we expect to simply switch to renewable sources while maintaining current demand. We need to encourage a less profligate approach to energy use, seeking greater efficiency and reducing waste.
Principle 7: Fossil fuels must be phased out as an energy source
Moving away from the fossil fuel-based economy is essential for the whole of society, though it is harder in some respects to make that transition in a rural landscape like the Quantock Hills. We need to do whatever we can to make it easier for businesses and residents here to reduce their dependency on fossil fuels, through renewables, reduced energy use, and more opportunities to share transport, for example.
Principle 8: We need a just transition to ensure no communities are negatively impacted
There is a massive societal shift required to respond to the climate crisis. That transition must be fair and equitable with the burden shared appropriately by all of us, according to our abilities and means. We must not allow the climate crisis to create new kinds of inequality.
Principle 9: The implementation must be democratic and involve all communities
Given the need for all parts of our communities to be part of the change, and given that climate change – and the transition to avoid it – affects all of us, the decision-making to enable change must include everyone.
Principle 10: We need to move beyond using economic growth as our measure of progress
We need to recognise as local communities and as a wider society, that our climate emergency is deepened by our continuing focus on economic growth as a measure of societal progress. A shift towards more progressive measures of a sustainable economy, based less on resource depletion and more on regenerative principles, would make the fight against climate change more winnable.
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5.3 Aims - Climate
That the distinctive geological diversity of the National Landscape is identifiable and understood; that potential climate change impacts are considered in respect of the resilience of the National Landscape’s special qualities.
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That the Quantock Hills National Landscape contributes to net zero through reduction of greenhouse gas emissions and provides sequestration and mitigation through appropriate land use and management.
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Photo: Woody dams installed as part of the Natural Flood Management project. © Quantock Hills National Landscape Team
5.4 Objectives – Climate
C1: To protect the carbon stores in the Quantock Hills and work to reduce emissions from the land, increasing carbon sequestration, ensuring this conserves or enhances the special qualities of the National Landscape.
C2: To promote nature-based actions to climate change that will deliver climate resilience and adaptation solutions enhancing existing priority habitats or enabling habitats to transition.
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5.5 Current status – Climate
5.5.1 Greenhouse gas emissions
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Data from Department for Energy Security and Net Zero 2024. Greenhouse gas emission data. See appendix 3 [pdf] for full data. The greenhouse gases covered by these statistics are carbon dioxide, methane and nitrous oxide.
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Between 2005 and 2022, the estimated total greenhouse gas emissions in the Quantock Hills National Landscape decreased from 22.3 to 10.8 ktCO2e – figures are expressed in kilotonnes of carbon dioxide equivalents. There were reductions in emissions in the following sectors:
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Industry 0.3 to 0.2 ktCO2e
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Commercial 1.7 to 0.8 ktCO2e
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Public sector 0.3 to 0.1 ktCO2e
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Domestic 9.0 to 4.3 ktCO2e
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Agriculture 17.7 to 14.8 ktCO2e
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Waste 1.3 to 0.2 ktCO2e
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The estimated total greenhouse gas emissions for Transport increased over the same time period from 9.5 to 9.6 ktCO2e.
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Land use, Land-use change and forestry (LULUCF) activities are a source of methane and nitrous oxide emissions AND a sink for carbon dioxide. Generally, emissions are produced from conversion of land to cropland and settlements and are removed through woodland / tree growth and conversion of arable to grassland. Emissions to the atmosphere are given as positive values, the removal of carbon, or equivalents, from the atmosphere is given as negative values. LULUCF emissions / sequestration values vary year on year from -17.5 (2005) to -20.0 (2010) ktCO2e and average at -19.0 ktCO2e.
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Over the same time period.
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Per capita emissions decreased from 9.6 to 4.1 tCO2e
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Per km2 emissions decreased from 0.2 to 0.1 ktCO2e
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5.5.2 Land use and carbon
In 2022 the National Landscape Association (NLA) commissioned Cranfield University to undertake a carbon audit and metric (land management) assessment for all National Landscapes. The project provided a baseline assessment of organic carbon storage capacity of habitats and of the fluxes – the overall capacity of a habitat to remove or release carbon from or to the atmosphere – for all 34 National Landscapes in England. The audit focused on carbon stocks and stores in the soils and biomass of priority and non-priority habitats within the National Landscapes. Along with a few additional sources, the audit was based on two main data sources:
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The NATMAP (the National Soils Map of England and Wales) carbon dataset which maps soil carbon stocks (at 1:250,000 scale).
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The literature available as summarised in Natural England’s research report Carbon Storage and Sequestration by Habitat 2021 – NERR094.
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The full data for the Quantock Hills National Landscape can be found in appendix 4 [pdf].
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Fieldwork was undertaken as part of the carbon audit comparing soil organic carbon contents represented by NATMAP carbon dataset to soil samples dug within three different National Landscapes – Blackdown Hills, Shropshire Hills and High Weald. This showed a strong correlation between the NATMAP data and the local soil samples. The Quantock Hills National Landscape Team have started soil sampling to assess the correlation at a local level of the NATMAP data which will give greater confidence using it for decision making and targeting of activity.
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For the Quantock Hills National Landscape:
Total soil carbon stored (0-150cm depth of soil) – 1,850,899 t C
Of this, priority habitats accounted for 804,325 t C and non-priority habitats for 1,046,575. The total carbon stored appears higher for non-priority habitat due to the larger geographical extent, at 6,633Ha compared to 3,276Ha for priority habitat (Figure 5). When considering carbon stocks – the amount of carbon contained within soils or biomass at a given time described in terms of tonnes per hectare [t C ha] – the figure for priority habitats is 246 t C ha compared to 158 t C ha for non-priority habitats. Figure c1 shows relative carbon stores by habitat type.
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Based on literature assessments the carbon flux – the overall capacity of a habitat to remove or release carbon from or to the atmosphere described in terms of tonnes of carbon per year – for the Quantock Hills National Landscape is -9,980.6 t C yr-1 . Negative figures represent carbon removal or sequestration. As would be expected there is significant variation between habitats with lowland meadows storing 5.2 tonnes carbon equivalent per hectare per year (t C ha-1 yr-1) and arable releasing 0.3 t C ha-1 yr-1. ​

Figure 5: Total carbon store (soil and biomass) in the Quantock Hills National Landscape by land use type / habitat.
5.6 Targets – Climate
Government has set targets for Protected Landscapes under the Protected Landscapes Targets and Outcomes Framework (see appendix 1 [pdf]). The Quantock Hills National Landscape will contribute to the following targets under the PLTOF:
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Target 6
Reduce net zero greenhouse gas emissions in Protected Landscapes to net zero by 2050 relative to 1990 levels.
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We do not currently have GHG emissions data for the Quantock Hills National Landscape at 1990 levels. However, we do have data from 2005 through to 2022 which shows a decrease in emissions from 22.3 to 10.8 kt CO2e.
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The Partnership should be looking at actions that will reduce GHG emissions and where the areas of greatest reduction could be. As with many other rural areas the significant contributors to GHG emissions are domestic, transport and livestock. Land use such as forestry and grasslands provide sequestration reducing the total GHG emissions for the National Landscape.
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Opportunities to reduce GHG, that are within the remit of the Partnership include agriculture, especially livestock, and improving soil sequestration, which is impacted by arable farming systems. Linking with targets 1, 7 and 8 will lead to a reduction in GHG emissions due to the increased sequestration these land uses provide.
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Quantock Hills Contribution towards the Target – Reduce net greenhouse gas emissions in the Quantock Hills to net zero by at least 2050 relative to 1990 levels.
Target 7
Restore approximately 130,000 hectares of peat in Protected Landscapes by 2050.
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This target is to be pro-rata’d for individual Protected Landscapes. For the Quantock Hills the baseline figure according to the Defra baseline figures is 14.87Ha. The extent of deep peat soils on the Quantock Hills is assessed as being in good condition. There is little opportunity to expand these areas and opportunities to create deep peat is constrained due to geology and shallow soils over much of the Quantock Hills. The Partnership agreed a target of 0Ha of new areas of deep peat but undertake actions that ensure the current extent of 14.87Ha is in favourable condition, or restored where degraded, by 2050.
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There is some scope for rewetting areas around acidic flushes, particularly downslope, and to block ditches / channels at higher elevations and on the upper parts of the small stream that flow from the hills to hold back water. This could result in conditions conducive to peat formation. There are pockets of deep peat on the hill, and this would serve to improve habitats as well as forming peat and reducing wildfire risk while reducing the downstream flooding.
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Quantock Hills Contribution towards the Target – 0Ha of new areas of deep peat, ensure current extent of 14.87Ha is in favourable condition, or restored where degraded by 2050.
Target 8
Increase tree canopy and woodland cover (combined) by 3% of total land area in Protected Landscapes by 2050 (from 2022 baseline).
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The current extent of woodland cover for the Quantock Hills National Landscape is 3,133 (31.69%), made up of 2,673.26Ha woodland and 460.72Ha tree cover outside of woodland. Due to the extent of existing woodland (3,133.98Ha) and other priority habitats (1,950.23Ha) along with higher agricultural land classification (grade 1 and 2) there is limited opportunities for large scale woodland creation. The Forestry Commissions Woodland Creation Sensitivity mapping (v4) identifies that 71% of the National Landscape is either unsuitable for woodland creation or has a high sensitivity meaning it would not usually be considered. Only 29% is medium sensitivity and there are no low sensitivity areas.
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There is however opportunity to work towards higher numbers of smaller plantings, such as field corners and increasing the number of trees in hedgerows. Using the Econet data we can use the stepping stone modelling to identify potential areas that would provide greatest connectivity achievable within the land use and landscape. This identifies 382Ha of potential woodland creation, such as small farm woodlands, field corners, enhancing hedgerows to create wooded corridors, etc and by cross referencing with the Woodland Creation Sensitivity mapping we can estimate 186Ha potential increase in tree cover.
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Quantock Hills Contribution towards the Target – Create 186Ha of new tree cover (woodland and outside woodland) within the Quantock Hills National Landscape bringing the total tree and woodland cover to 33.57%.
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5.7 Policies – Climate
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CL1: Support initiatives and actions that allow farmers / landowners to reduce Greenhouse Gas (GHG) emissions and maximise carbon storage such as regenerative farming systems or tree planting or restoration of soils, that will conserve or enhance the special qualities of the National Landscape.
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CL2: Support Quantock Hills National Landscape communities, business and individuals to collectively make changes to their behaviour, such as energy, transport and food to transition to net zero.
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CL3: Support initiatives that promote the transition to low carbon and renewable energy in a way that furthers the conservation and enhancement of the special qualities of the Quantock Hills National Landscape.
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CL4: Support initiatives that promote the active travel approach for local communities and users of the Quantock Hills National Landscape.
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CL5: Support initiatives that undertake actions that will enhance priority habitat / species resilience and ability to adapt to climate change in a way which supports or furthers the special qualities of the Quantock Hills such as nature-based solutions and natural flood management.
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