Subsidence cases across the UK are increasingly linked to climate change, with rising risks especially acute in areas overlaying shrinkable clay soils such as London clay. The southeast of England, and London in particular, faces a heightened threat due to its dense urban fabric, clay-heavy ground conditions, and vulnerability to extreme weather events including heatwaves and droughts.

A report commissioned by London Mayor Sadiq Khan warns that over 40% of homes in the capital could be affected by subsidence as early as 2030, up from 20% in 1990. Projections indicate this figure could reach 57% by 2070, reflecting a significant climb in the number of properties exposed to ground movement caused by climatic shifts. Similarly, the British Geological Survey highlights a national trend wherein the proportion of buildings at high or extreme risk of "shrink-swell" subsidence is expected to more than double by 2030 and rise to approximately 10% of all properties by 2070. London boroughs, especially northern and central areas, represent prime hotspots within the UK.

The underlying cause stems from changes in soil moisture as hotter, drier summers lead to ground shrinkage, especially in clay soils. This shrinkage results in cracks and structural movement beneath buildings, an issue compounded by successive subsidence surge events declared after record hot summers in recent years. The insurance sector has noted a sharp escalation in claim volumes related to subsidence in London, with expectations of a 57.3% rise in claims by 2070, carrying potential financial impacts nearing £1.9 billion.

Heritage sites are among the most vulnerable to these climate-induced geological changes, with conservation efforts particularly challenged by the lack of prior examples and clear precedents. One illustrative case is St John the Evangelist Church in Upper Norwood, London—a Grade II* listed red brick Gothic Revival building constructed on London clay. This church has endured significant subsidence, manifesting in severe structural cracks, threatening historic features like the south aisle and necessitating the reconstruction of important interior elements such as the rood screen.

The church has become the focus of a comprehensive project employing physically-based modelling to analyse the causes of structural movement. This effort aims to support stakeholders in devising adaptive conservation plans responsive to evolving climate risks. Over £700,000 has been invested in remedial works, including underpinning the vulnerable south wall, funded through coordinated grants including from the Heritage Lottery Fund. These actions have stabilised the building and enabled ongoing restoration of interior damage, positioning the church better for future preservation in the context of climate change.

The challenges facing St John the Evangelist are emblematic of broader pressures on built heritage and residential properties alike, underscoring the urgent need for informed and proactive adaptation strategies. London, often highlighted as a subsidence hotspot due to its shrinkable clay soils combined with urban density, highlights the complex interplay of climate dynamics, geology, and built environment vulnerabilities that will require multifaceted responses by policymakers, insurers, engineers, and conservationists moving forward.

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Source: Noah Wire Services