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- Q5138350 subject Q15088885.
- Q5138350 abstract "Coastal flooding occurs when normally dry, low-lying land is flooded by sea water. The extent of coastal flooding is a function of the elevation inland flood waters penetrate which is controlled by the topography of the coastal land exposed to flooding. The sea water can inundate the land via several different paths:Direct inundation — where the sea height exceeds the elevation of the land, often where waves have not built up a natural barrier such as a dune systemOvertopping of a barrier — the barrier may be natural or human engineered and overtopping occurs due to swell conditions during storm or high tides often on open stretches of the coast. The height of the waves exceeds the height of the barrier and water flows over the top of the barrier to flood the land behind it. Overtopping can result in high velocity flows that can erode significant amounts of the land surface which can undermine defense structures.Breaching of a barrier — again the barrier may be natural or human engineered, and breaching occurs on open coasts exposed to large waves. Breaching is where the barrier is broken down by waves allowing the sea water to extend inland.Coastal flooding is largely a natural event, however human influence on the coastal environment can exacerbate coastal flooding. Extraction of water from groundwater reservoirs in the coastal zone can enhance subsidence of the land increasing the risk of flooding. Engineered protection structures along the coast such as sea walls alter the natural processes of the beach, often leading to erosion on adjacent stretches of the coast which also increases the risk of flooding.".
- Q5138350 wikiPageExternalLink %28ASCE%29WR.1943-5452.0000036.
- Q5138350 wikiPageExternalLink globalfloodmap.org.
- Q5138350 wikiPageExternalLink Hunt_ClimateChange_2011_104_1_13.pdf.
- Q5138350 wikiPageExternalLink EM_1998_52.pdf.
- Q5138350 wikiPageExternalLink coastal-hazards-climate-change-guidance-manual.pdf.
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- Q5138350 comment "Coastal flooding occurs when normally dry, low-lying land is flooded by sea water. The extent of coastal flooding is a function of the elevation inland flood waters penetrate which is controlled by the topography of the coastal land exposed to flooding.".
- Q5138350 label "Coastal flood".