Coastal flooding occurs when dry and low-lying land is submerged () by seawater.
Coastal plain are sometimes flooded by unusually high tides, such as , especially when compounded by high winds and . This was the cause of the North Sea flood of 1953 which flooded large swathes of the Netherlands and the East coast of England.
When humans modify the coastal environment this can make coastal flooding worse.
Reduction and control of coastal flooding is carried out using structural methods to hold back or redirect flood waters. Non-structural methods include coastal management, behavioral and institutional response to adapt to the processes. Natural defenses include physical features like gravel bars and sand dune systems, but also ecosystems such as salt marshes, seagrass and mangrove forests which have a buffering function. , wetlands and Seagrass meadow are often considered to provide significant protection against storm waves, tsunamis, and shoreline erosion through their ability to attenuate wave energy.
Types
The
seawater can flood the land via several different paths:
-
Direct flooding — where the sea height exceeds the elevation of the land, often where waves have not built up a natural barrier such as a dune
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Overtopping of a barrier — the barrier may be natural or human-engineered and overtopping occurs due to swelling conditions during storms or high tides often on open stretches of the coast.
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Breaching of a barrier — again the barrier may be natural (sand dune) or human-engineered (sea wall), and breaching occurs on open coasts exposed to large waves. Breaching occurs when the barrier is broken down or destroyed by waves allowing the seawater to extend inland and flood the areas
Causes
Coastal flooding can result from a variety of different causes including
created by storms like
and
, rising sea levels due to climate change and
. in 1954]]
Storms and storm surges
Storms, including
hurricanes and tropical cyclones, can cause flooding through
storm surges which are waves significantly larger than normal.
If a storm event coincides with the high astronomical tide, extensive flooding can occur.
Storm surges involve three processes:
-
wind setup
-
barometric setup
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wave setup
Wind blowing in an onshore direction (from the sea towards the land) can cause the water to 'pile-up' against the coast; this is known as wind setup. Low atmospheric pressure is associated with storm systems and this tends to increase the surface sea level; this is a barometric setup. Finally increased wave breaking height results in a higher water level in the surf zone, which is wave setup. These three processes interact to create waves that can overtop natural and engineered coastal protection structures thus penetrating seawater further inland than normal.
Sea level rise
Tidal flooding
Tsunami waves
Coastal areas can be significantly flooded as the result of
tsunami waves
which propagate through the
ocean as the result of the displacement of a significant body of water through
earthquakes,
landslides, volcanic eruptions, and
glacier calvings. There is also evidence to suggest that significant tsunami have been caused in the past by
meteor impact into the ocean.
Tsunami waves are so destructive due to the
velocity of the approaching waves, the height of the waves when they reach land, and the
debris the water entrains as it flows over land can cause further damage.
Depending on the magnitude of the tsunami waves and floods, it could cause severe injuries which call for precautionary interventions that prevent overwhelming aftermaths. It was reported that more than 200,000 people were killed in the earthquake and subsequent tsunami that hit the Indian Ocean, on December 26, 2004.
Impacts
Social and economic impacts
The
coastal zone (the area both within 100 kilometres distance of the coast and 100 metres elevation of sea level) is home to a large and growing proportion of the global population.
Over 50 percent of the global population and 65 percent of cities with populations over five million people are in the coastal zone.
In addition to the significant number of people at risk of coastal flooding, these coastal urban centres are producing a considerable amount of the global Gross Domestic Product (GDP).
People's lives, homes, businesses, and city infrastructure like roads, railways, and industrial plants are all at risk of coastal flooding with massive potential social and economic costs.
Environmental impacts
Coastal flooding can result in a wide variety of environmental impacts on different spatial and temporal scales. Flooding can destroy coastal habitats such as coastal
wetlands and
estuaries and can erode dune systems.
These places are characterized by their high biological diversity therefore coastal flooding can cause significant biodiversity loss and potentially species
extinctions.
In addition to this, these coastal features are the coasts natural buffering system against storm waves; consistent coastal flooding and sea-level rise can cause this natural protection to be reduced allowing waves to penetrate greater distances inland exacerbating erosion and furthering coastal flooding.
"By 2050, “moderate” (typically damaging) flooding is expected to occur, on average, more than 10 times as often as it does today, and can be intensified by local factors."
Prolonged inundation of seawater after flooding can also cause salination of agriculturally productive soils thus resulting in a loss of productivity for long periods of time.
Reduction and control
Flood control
Non-structural mechanisms
If human systems are affected by flooding, an adaption to how that system operates on the coast through behavioral and institutional changes is required, these changes are the so-called
non-structural mechanisms of coastal flooding response.
Building code, coastal hazard zoning, urban development planning, spreading the risk through insurance, and enhancing public awareness are some ways of achieving this.
A more extreme and often difficult to accept the response to coastal flooding is abandoning the area (also known as managed retreat) prone to flooding.
Engineered defenses
There are a variety of ways in which humans are trying to prevent the flooding of coastal environments, typically through so-called hard engineering structures such as
,
seawalls and
levees.
That armouring of the coast is typical to protect towns and cities which have developed right up to the beachfront.
Enhancing depositional processes along the
coast can also help prevent coastal flooding. Structures such as
groynes,
breakwaters, and artificial headlands promote the deposition of sediment on the beach thus helping to buffer against storm waves and surges as the wave energy is spent on moving the sediments in the beach than on moving water inland.
Natural defenses
Coastal areas do provide natural protective structures to guard against coastal flooding. These include physical features like
gravel bars and
sand dune systems, but also
ecosystems such as
salt marshes,
seagrass and
mangrove forests have a buffering function.
,
wetlands and
Seagrass meadow are often considered to provide significant protection against storm waves, tsunamis, and shoreline
erosion through their ability to attenuate wave energy.
To protect the coastal zone from flooding, the natural defenses should, therefore, be protected and maintained in for example Marine Protected Areas (MPAs).
Longer term aspects and research
Reducing global sea level rise is one way to prevent significant flooding of coastal areas. This could be minimised by further reducing greenhouse gas emissions. However, even if significant emission decreases are achieved, there is already a substantial amount of sea level rise into the future.
International climate change policies like the
Paris Agreement are seeking to mitigate the future effects of climate change, including sea level rise. In addition, more immediate measures of engineered and natural defenses are put in place to prevent coastal flooding.
Examples
Examples of countries with existing coastal flooding problems include:
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The Netherlands: Flood control in the Netherlands
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Bangladesh: Floods in Bangladesh
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Great Britain: The Thames Barrier is one of the world's largest flood barriers and serves to protect London from flooding during exceptionally high tides and storm surges.
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New Zealand: Flooding of the low-lying coastal zone South Canterbury Plains in New Zealand can result in prolonged inundation, which can affect the productivity of the affected pastoral agriculture for several years.
-
The Caribbean:
Hurricane Katrina in New Orleans
Hurricane Katrina made landfall as a category 3
cyclone on the Saffir–Simpson hurricane wind scale, indicating that it had become an only moderate level storm.
However, the catastrophic damage caused by the extensive flooding was the result of the highest recorded storm surges in
North America.
For several days prior to the landfall of Katrina, wave setup was generated by the persistent winds of the cyclonic rotation of the system. This prolonged wave set up coupled with the very low central pressure level meant massive storm surges were generated.
Storm surges overtopped and breached the
levees and floodwalls intended to protect the city from inundation.
Unfortunately,
New Orleans is inherently prone to coastal flooding for a number of factors. Firstly, much of New Orleans is below sea level and is bordered by the Mississippi River therefore protection against flooding from both the sea and the river has become dependent on engineered structures.
Land-use change and modification to natural systems in the Mississippi River have rendered the natural defenses for the city less effective.
Wetland loss has been calculated to be around since 1930. This is a significant amount as four miles of wetland are estimated to reduce the height of a
storm surge by one foot (30 centimeters).
Indonesia and Japan earthquake-related tsunamis
2004 Indian Ocean earthquake and tsunami: An
earthquake of approximately magnitude 9.0 struck off the coast of
Sumatra,
Indonesia causing the propagation of a massive
tsunami throughout the
Indian Ocean.
This tsunami caused significant loss of human life, an estimate of 280,000 – 300,000 people has been reported
and caused extensive damage to villages, towns, and cities and to the physical environment. The natural structures and habitats destroyed or damaged include
coral reefs, mangroves, beaches, and seagrass beds.
The more recent earthquake and tsunami in
Japan in March 2011 (2011 Tōhoku earthquake and tsunami) also clearly illustrates the destructive power of tsunamis and the turmoil of coastal flooding.
See also
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Coastal flood advisory, watch, warning (U.S.)
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Coastal management
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Flash flood
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Saltwater intrusion
Sources
