HomeGround › The clay forecast
Britain's clay just had its two driest summers in 26 years, back to back. Expect a subsidence-claims surge.
Subsidence claims in Britain follow dry summers on shrink–swell clay: the ground dries, shrinks, and the houses on it move. In the satellite soil-moisture record, summer 2026 is the driest of 26 years over the high-risk clay (index -2.40), and summer 2025 was second driest (-1.78) — clay entered this year already desiccated. The same index, computed the same way, back-predicts the documented claim surges: 2022 — which the ABI says produced 23,000 subsidence claims and a £219m expected bill - the highest since 2006 — ranks 3 of 26; 2006 ranks 5; 2018 ranks 6; the quiet wet summers stay at the bottom. So we are saying it plainly, on 2026-08-07: the coming claims period should be an elevated one — direction and scale, never a precise count, because a wet autumn can still blunt it (and a dry one deepen it: 2003's surge came from an autumn drought alone). The measurements are a satellite-informed model reanalysis — the same instrument for every year — not probes in the ground; industry claim figures are the ABI's, quoted and linked, not ours. When the outcome is published, we will append it here, right or wrong.
summer 2026's dryness rank on Significant clay (1 = driest)
summer 2025's rank — the back-to-back that compounds it
documented surge summers back-predicted (the fourth was an autumn event, shown below)
grid cells nationwide where 2026 is the driest summer on record
Every year, same instrument, same clay
The clay-drought index: mean soil-moisture z-score across the 392 BGS Significant shrink–swell hexes, 1 June - 5 August window, 2001-2020 baseline. Lower is drier. Surge years marked from the industry's own record.
| Rank | Year | Index | Known for |
|---|---|---|---|
| 1 | 2026 | -2.40 | this summer — the forecast |
| 2 | 2025 | -1.78 | last summer — the set-up |
| 3 | 2022 | -1.48 | documented claim-surge summer |
| 4 | 2011 | -1.25 | |
| 5 | 2006 | -1.08 | documented claim-surge summer |
| 6 | 2018 | -0.83 | documented claim-surge summer |
| 7 | 2010 | -0.82 | |
| 8 | 2017 | -0.72 | |
| 9 | 2020 | -0.65 | |
| 10 | 2015 | -0.61 | |
| 11 | 2019 | -0.61 | |
| 12 | 2005 | -0.57 | |
| 13 | 2009 | -0.47 | |
| 14 | 2023 | -0.45 | |
| 15 | 2014 | +0.20 | |
| 16 | 2004 | +0.22 | |
| 17 | 2013 | +0.44 | |
| 18 | 2008 | +0.53 | |
| 19 | 2003 | +0.90 | surge year — drought arrived in autumn (rank 4 in Aug–Oct) |
| 20 | 2012 | +0.92 | quiet wet summer (control) |
| 21 | 2002 | +0.98 | |
| 22 | 2016 | +1.04 | |
| 23 | 2024 | +1.06 | quiet wet summer (control) |
| 24 | 2021 | +1.18 | |
| 25 | 2001 | +1.20 | |
| 26 | 2007 | +1.20 | quiet wet summer (control) |
Where the dry clay is
The 20 driest districts of the 110 holding Significant shrink–swell clay, by this summer's index. A caution that keeps us honest: z-scores run large where summers are normally wet, so compare within the table, not against other datasets — and note the same districts were already dry in 2025.
| District | Clay hexes | Summer 2026 | Summer 2025 |
|---|---|---|---|
| Folkestone and Hythe | 2 | -5.38 | -2.37 |
| Ashford | 1 | -5.38 | -2.37 |
| North Yorkshire | 18 | -4.18 | -2.32 |
| North Lincolnshire | 2 | -4.07 | -2.43 |
| West Lindsey | 6 | -3.76 | -2.33 |
| Bournemouth, Christchurch and Poole | 3 | -3.43 | -1.16 |
| Swale | 4 | -3.41 | -2.48 |
| Canterbury | 2 | -3.41 | -2.48 |
| Southend-on-Sea | 1 | -3.41 | -2.48 |
| Colchester | 5 | -3.24 | -2.12 |
| Tendring | 6 | -3.24 | -2.12 |
| Babergh | 4 | -3.24 | -2.12 |
| East Suffolk | 5 | -3.24 | -2.12 |
| Ipswich | 1 | -3.24 | -2.12 |
| Eastbourne | 1 | -3.16 | -1.83 |
| Tonbridge and Malling | 1 | -3.16 | -1.83 |
| Isle of Wight | 7 | -3.14 | -1.15 |
| Dorset | 18 | -3.13 | -1.33 |
| Maldon | 7 | -2.82 | -2.05 |
| Somerset | 5 | -2.80 | -1.64 |
Download: the full index by year (CSV) · the district table (CSV).
Method — so the forecast can be checked, now and next year
- Soil moisture: NASA POWER root-zone wetness (GWETROOT, MERRA-2 — satellite-informed model reanalysis), daily, 0.5° grid over England and Wales, 2001–2026. The window is 1 June - 5 August because that is where 2026's data currently ends — every year is scored on the identical window.
- Clay: the 392 hexes where BGS GeoSure rates shrink–swell susceptibility Significant (the same layer our property reports use). The index is the mean z-score over those hexes; z against the 2001-2020 baseline.
- Hindcast before forecast: the documented surge summers must rank dry (2022: 3, 2006: 5, 2018: 6) and the quiet wet summers must rank wet — they do. The exception is 2003, whose drought was an autumn event (2003's desiccation was an autumn event - documented, not hidden).
- The claim-surge record is the insurance industry's own: ABI, March 2023 — “23,000 subsidence claims and a £219m expected bill - the highest since 2006”. Quoted, not re-tabulated.
- The receipt: this page is dated 2026-08-07. When the industry publishes the coming period's subsidence figures, the outcome gets appended here — right or wrong.
Related: Sinking Britain — where the ground is already moving, measured; the paid UK property report carries measured ground motion and clay susceptibility for a single address. We did not produce the measurements; we produced the join.
Is my house about to crack?
Almost certainly not — most homes, even on clay, come through dry years fine. This is an area-level forecast about how many claims the insurance industry should expect, not a prediction for any building. Clay-related damage develops over months and shows up as new or widening cracks, typically around openings; if you see that, the sensible steps are photographs, dates, and your insurer — not panic. Our paid report includes measured ground motion and clay susceptibility for a specific address.
Why should anyone trust a forecast?
Because we tested it backwards before publishing it forwards. The same index — satellite-era soil moisture over the same high-risk clay, the same summer window — scores the documented surge summers of 2022 (rank 3), 2006 (rank 5) and 2018 (rank 6) among the driest, and scores the quiet wet summers as wet. One known surge year, 2003, does not light up in the summer window — because its drought arrived in the autumn (August–October, where it ranks 4th driest). We publish that exception rather than hiding it.
What could make this forecast wrong?
Rain, mostly. A wet autumn can rehydrate clay before damage compounds — it blunted the aftermath of 2018 — while a dry autumn deepens it, which is how 2003 produced a surge on its own. Claims also lag: cracks from this summer surface over winter and into next year, and insurer thresholds and reporting behaviour move the numbers. That is why the forecast is about direction and scale — an elevated claims period — never a precise count.
What exactly did you measure?
NASA POWER root-zone soil wetness (GWETROOT) — a satellite-informed model reanalysis, not a probe in the ground — averaged over 1 June - 5 August each year from 2001, scored against the 2001-2020 baseline, then averaged over the 392 five-kilometre hexes where BGS rates shrink–swell susceptibility Significant. Model reanalysis is the honest label: it is the same instrument for every year, which is what a fair comparison needs.
Novarly Parcel · official public data, read properly · parcel.novarly.com
A forecast is a statement of elevated likelihood, not fate: screening-grade analysis from public data, not advice for any property, policy or claim. Methodology · The ground under the sea-level record