Coastal Flooding
- Coastal flooding results from a number of factors:
- Storm surges: a rapid rise in sea level caused by really low-pressure storms (e.g. tropical storm)
- Storm tides: occur when there is a combination of high tide and low-pressure storm
- Tsunamis: large sea waves due to underwater earthquakes. The closer to the coast, the bigger the impact
- King tides
- Sea level rise due to sea temperatures increase from global warming, putting low-lying coastal land at increased risk of flooding
- High river discharge after a storm: when combined with a spring tide, water in the estuary cannot discharge into the sea causing a backflow of water and flooding
- Global warming and climate change is increasing the frequency and intensity of storms through increased evaporation and rainfall
- This increases the height and strength of waves and increases weathering, erosion and mass movement
- Erosion may increase which adds to coastal retreat and risk of further cliff collapse
- Depositional features such as spits and bars can be destroyed
- Impacts are varied from moving people from towns and villages to defences against storm surges and rising tides
- Flooding of roads and damage to railways make travel difficult and are expensive to repair
- The worst flooding arises from a combination of any of these
- The biggest impacts are felt by emerging countries, although the biggest economic cost is are to developed countries
Exam Tip
Areas most at risk for coastal flooding in the UK include:
- East Anglia
- Towyn and Rhyl, North Wales
- Aberystwyth, Mid Wales
- Liverpool
- Carlisle
- Holderness Coastline
- Jurassic Coastline
- Bristol