Coastal Flooding Explained
Understanding coastal flooding in England — tidal surges, storm surges, and sea level rise.
Last updated: 2026-03-28
How Coastal Flooding Happens
Coastal flooding occurs when the sea level temporarily rises above normal, overtopping or breaching sea defences.
Key Causes
- Storm surges: Low atmospheric pressure and strong winds push sea levels up by 1-2 metres or more
- High tides: Spring tides are naturally higher; combined with a surge, they create extreme levels
- Wave overtopping: Large waves crash over sea walls
- Sea level rise: Long-term climate change is raising average sea levels
- Coastal erosion: Weakened coastline is more vulnerable
Most At-Risk Areas
- The east coast (North Sea surge corridor)
- The Severn Estuary (tidal range of up to 14 metres)
- The Humber Estuary
- Low-lying areas behind sea defences
- Reclaimed land (the Fens, Romney Marsh, Somerset Levels)
The 1953 North Sea Flood
The UK's worst coastal flood killed 307 people and led to the creation of the modern flood warning system and the Thames Barrier.
Sea Level Rise
Sea levels around England are rising by about 3-4mm per year. The EA's climate change allowances add up to 1.2 metres to design flood levels for coastal developments.
Coastal Defences
England has about 3,000 km of coastal flood defences including sea walls, embankments, groynes, and managed realignment areas.