Storm surge hits UK Coastline

A storm surge on 3 Jan 2014 in the Irish Sea (similar to the recent one on 5 December 2013) raised the sea surface above the astronomical tide level by 0.75 metres to 1 metre over a large area.

Storm surges occur when strong winds push water up against a coastline. Low atmospheric pressure associated with weather systems causes the sea level to rise even further. Serious coastal flooding often occurs when storm surges coincide with large spring tides.

Storm surge models

NOC scientists have developed computer models to predict the occurrence of storm surges. These models run on supercomputers at the UK Met Office and are a critical part of today’s coastal flood warning system.

Liverpool surge model, tidal observations and predictions for 3 Jan 2014

As in the surge of December 2013, our model runs predicted the surge and its approximate height (see plot below).

Computer model runs predict the 0.8m high storm surge

The near real-time data from the tide gauge at Liverpool show the predicted tide level and the observed clearly showing the surge (see plot below).

Tidal observations show the storm surge increase compared with predicted height

Visit the National Tidal and Sea Level Facility website for more observations, predictions and information.

Photographs of storm surge in Irish Sea on 3 Jan 2014

Storm surge at New Brighton, Wirral coast Storm surge at New Brighton, Wirral coast Storm surge at New Brighton, Wirral coast Storm surge at New Brighton, Wirral coast Storm surge at New Brighton, Wirral coast Storm surge at New Brighton, Wirral coast Storm surge at New Brighton, Wirral coast Storm surge at New Brighton, Wirral coast

Liverpool surge model, tidal observations and predictions for 5 December 2013

Computer model runs predict the 1m high storm surge

Tidal observations show the storm surge increase compared with predicted height

Visit the National Tidal and Sea Level Facility website for more observations, predictions and information.

Photographs of storm surge in Irish Sea on 5 December 2013

The impacts of the storm surge could be seen at Hoylake in Wirral, close to NOC's Liverpool Centre -

Storm surge at Hoylake, Wirral coast Storm surge at Hoylake, Wirral coast Storm surge at Hoylake, Wirral coast Storm surge at Hoylake, Wirral coast Storm surge at Hoylake, Wirral coast Storm surge at Hoylake, Wirral coast Storm surge at Hoylake, Wirral coast

Video of storm surge in Irish Sea

Lowestoft surge model, tidal observations and predictions

Overnight on the 5–6th December 2013 the east coast of the UK took a battering from high winds and storms surges. NOC model runs and tidal observations show the 2m storm surge at Lowestoft in Suffolk.

Surge model predicts 2m increase in water level

Tidal observations show the storm surge increase compared with predicted height

The storm surge of 1953

During the night of 31 January 1953, coastal flooding caused the loss of 307 lives in East Anglia. The same event was responsible for a further 1795 fatalities in the Netherlands. The disaster prompted the British government to install the Thames Barrier. The Dutch commissioned a vast coastal defence project called The Delta Works.

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