Coastal Management (Cambridge (CIE) IGCSE Geography)
Revision Note
Written by: Jacque Cartwright
Reviewed by: Bridgette Barrett
Managing the Impacts of Coastal Erosion
There are conflicting views about what type of engineering to use for coastal defence
Most coastal managers aim to use a range of methods depending on the value of what is being protected
This method is known as Integrated Coastal Zone Management (ICZM)
ICMZ aims to use a combination of methods to best reflect all stakeholder's needs
Soft engineering methods
Soft engineering works with natural processes rather than against them
Usually cheaper and do not damage the appearance of the coast
Considered a more sustainable approach to coastal protection
However, they are not as effective as hard engineering methods
Soft-engineered defences
Beach replenishment
This is the pumping or dumping of sand and shingle back onto a beach to replace eroded material
Advantages
Beaches absorb wave energy
Widens beachfront
Disadvantages
Has to be repeated regularly, which is expensive
Can impact sediment transportation down the coast
Fencing, hedging, and replacing vegetation
Helps to stabilise sand dunes or beaches
Reduces wind erosion
Advantages
Cheap method to protect against flooding and erosion
Disadvantages
Hard to protect larger areas of coastal cliffs
Cliff re-grading
This is when the angle of a cliff is softened to reduce mass movement
Advantages
Prevents the sudden loss of large sections of cliff
As wave energy is slowed, wave-cut notching is reduced at the base of the cliff
Disadvantages
It does not stop cliff erosion; it only slows it down
Beach re-profiling
Beach reprofiling is the artificial re-shaping of a beach using existing beach material
Advantages
Replaces shingle after winter storms
Increasing the profile reduces wave energy before the base of the cliffs
Disadvantages
Reprofiling may have a negative effect on beach habitats
Managed retreat
The existing coastal defences are abandoned, allowing the sea to flood inland until it reaches higher land or a new line of defences
Advantages
There are no expensive construction costs
Creates new habitats such as salt marshes
Disadvantages
Disruptive to people where land and homes are lost
The cost of relocation can be expensive
Full compensation to people and businesses may not be paid
Hard engineering methods
Hard engineering involves building concrete, wood, or rock sea defences
Building and maintaining structures is costly
Defences work against the power of the waves
Each defence has pros and cons
Protection in one place can increase erosion and flooding along the coast
When settlements and expensive installations (power stations, etc) are under risk, hard engineering is used because the economic gain outweighs the costs
Hard-engineered defences
Sea wall
A sea wall is usually concrete and curved outwards to deflect the power of the waves
Advantages
Most effective at preventing both erosion and flooding (if the wall is high enough)
Disadvantages
Very expensive to build and maintain
It can be damaged if the material in front of the wall is not maintained
Restricts access to the beach
Unsightly to look at
Groynes
These are wood, rock or steel pilings that are built at right angles to the shore
Longshore drift moves beach material into groynes
Advantages
Most effective at preventing both erosion and flooding (if the wall is high enough)
Disadvantages
Keeps material from moving down the coast and protects cliff bases elsewhere
Starves other beaches of sand
Wooden groynes need maintenance to prevent wood rot
Makes walking along the shoreline difficult
Rip-rap or rock armour
Large boulders are piled up to protect a stretch of coast
Works to absorb wave energy from the base of cliffs and sea walls
Advantages
Cheaper method of construction
Disadvantages
Boulders can be eroded or dislodged during heavy storms
Gabions
Wire cages are filled with stone, concrete, sand, etc.
Cages absorb wave energy
Advantages
Cheapest form of coastal defence
Can be stacked at the base of a sea wall or cliffs
Disadvantages
Wire cages can break, and they need to be securely tied down
Not as efficient as other coastal defences
Revetments
Sloping wooden or concrete fence with an open plank structure
Revetments work to break the force of the waves
Advantages
Traps beach material behind them
Set at the base of cliffs or in front of the sea wall
Cheaper than sea walls but not as effective
Disadvantages
Not effective in stormy conditions
Can make beach inaccessible for people
Regular maintenance is necessary
Visually unattractive
Off-shore barriers
Large concrete blocks, rocks and boulders are sunk offshore to alter wave direction and weaken wave energy
Advantages
Beach material is built up
Low maintenance
Maintains natural beach appearance
Disadvantages
Expensive to build
Can be removed in heavy storms
Can be unattractive
Prevents surfing and sailing
Prediction
Early warning systems allow communities to prepare (evacuate or take shelter) before flooding occurs
Two methods are used to help forecast coastal flooding
Past records: diaries, newspapers, government/council records, etc.
These identify areas that are at high risk of flooding and their frequency
Modern technology: GIS, satellite and computer monitoring, weather stations (local and national), etc.
These forecast and track potential hazardous events such as:
Tropical storms: track the storm's path and associated storm surge
Earthquakes: the size and position of underwater tremors and possible tsunami outcome
Both forecasting methods help officials determine when and where the event will occur
They shows the risk of damage and fatalities as well as the potential intensity and scope of the flooding
Prevention
Prevention is about taking action that reduces or removes the risk of coastal flooding
Actions include:
Flood defences
These are built along high-risk stretches of coast
Emergency centres
Centrally placed on higher ground where people can be safe from flooding
Early warning systems
Allows for preparation or evacuation of an area
Education
Informing local people on what to do if and when a flood occurs
Planning
Any new development should be planned away from high-risk-areas
Design buildings to deal with low levels of flooding
Raise buildings to allow floodwaters to flow underneath
Strengthen barriers
Sealing a property to prevent floodwater intrusion is known as dry floodproofing
Wet flood proofing allows some flooding of the building
Buffer zones
Areas of land are allowed to flood before reaching settlements
This slows down the floodwater's journey by allowing the surge's energy to dissipate
It can mean moving people away from the coast, which could be controversial
Coastal strategies
Management of coastal regions is performed by identifying coastal cells
This breaks a long coastline into manageable sections and helps identify two related risks:
The risk of erosion and land retreat
The risk of flooding
Identifying risks allows resources to be used efficiently to limit their impacts
The 'cost to benefit' is easier to calculate using coastal cells
Shoreline management plans
Shoreline management plans (SMPs) outline strategies to prevent flooding and erosion along a coastline
The strategies try to limit the risk to people, settlements, agricultural land, and natural habitats (such as salt marshes)
There are four ways to manage coastal areas, each with different costs and consequences
Hold the line
This is a long-term approach and the most costly
It involves building and maintaining coastal defences to keep the current position of the shoreline
Dominated with hard engineering with soft engineering supporting it
Advance the line
New defences are built to extend the existing shoreline
Involves reclaiming land
Hard and soft engineering is used
Managed realignment
The coastline is allowed to move naturally
Processes are monitored and directed when and where necessary
The most natural approach to coastal defence
Mostly soft engineering with some hard engineering to support
Do nothing
The cheapest method, but also the most controversial of the options
The coast is allowed to erode and retreat inland
No investment is made in protecting the coastline or defending against flooding, regardless of any previous intervention
Decisions about which approach to use are complex and depend on:
Economic value of the resources that would be protected, e.g. land, homes, etc
Engineering solutions: it might not be possible to 'hold the line' for moving landforms such as spits or unstable cliffs
Cultural and ecological value of land: historic sites and areas of unusual diversity
Community pressure: are there any local campaigns to protect the region?
The social value of communities: long-standing, historic communities
Worked Example
Explain how gabions protect the coast
[2 marks]
Solution
Gabions absorb/dissipate/reduce the wave's energy/power [1 mark]. This reduces the impact of the waves at the foot of cliffs and seawalls, which reduces/prevents coastal erosion [1 mark].
Marking guidance
The command word here is 'explain,' and answers need to be developed for full marks.
1 mark for identifying the purpose
1 mark for development
Case Study: Super Typhoon Haiyan
Managing tropical storms is difficult due to the unpredictability of their paths
The distribution of the population along a coast increases the risk associated with tropical storms
The strength of the storm does not always cause the most damage; developing countries are usually the worst affected
Preparedness is an effective way of managing tropical storms
Hazard mitigation relies on effective response to natural events
Background
Typhoon Haiyan (Yolanda) was one of the strongest tropical storms to hit the Philippines
It made landfall on November 8, 2013, as a Category 5 with sustained winds above 195 mph
The Philippines are a group of South China Sea islands located east of Vietnam and north of Indonesia
Southwest typhoons regularly sweep in every tropical storm season
Even though the islands sit in warm ocean water, the storm's sea temperature at the time was 30 °C
Since 1900, sea levels have risen 20 cm around the world. Higher seas are known to contribute to stronger storm surges
Over-abstraction of groundwater has caused parts of the country to sink
Tacloban stands at the end of a bay that is funnel-shaped and this squeezes water into destructive storm surges
Formation of tropical storms
All tropical storms need:
warm, deep water (>27°C and >70 m depth)
sufficient spin from the earth’s rotation (Coriolis force)
This is why they form between 5-20° N and S of the equator
Warm water encourages sea surface evaporation, while rising air cools, condenses, releases latent heat, and produces large thunderclouds
The heat from below produces vertical growth and intense low-pressure
Tropical storms form when several storms merge at the eastern side of an ocean
A major low-pressure cell develops and as winds are drawn in, the whole system begins to spin anticlockwise and westward
Winds rotate around a central eye, where cold air descends, creating an area of calm
The strongest winds are within the eyewall
Typhoon Haiyan's timeline
Nov 2013
2nd: an area of low pressure develops several hundred kilometres east of Micronesia
3rd: Haiyan begins to track westward, deepening into a tropical depression
5th: The Philippines Atmospheric, Geophysical, and Astronomical Services Administration (PAGASA) classified it as a typhoon and issued a low-level public storm warning
6th: declared a Category 5 super typhoon by the Joint Typhoon Warning Centre. PAGASA raises storm warning to highest level, indicating expected wind speeds in excess of 115 mph
7th: Haiyan's winds continue to intensify up to 195 mph. Haiyan makes first landfall at Guiuan, Eastern Samar, without losing any intensity
8th: Haiyan makes five more landfalls within the Philippines before passing into the South China Seas
10th: Haiyan turns to the NW and makes landfall in Northern Vietnam as a Category 1 typhoon
11th: Haiyan finally weakens into a tropical depression
Typhoon Haiyan's characteristics
Lowest pressure: 895 mb
Peak strength: category 5
Strength at landfall: Category 5 with 195 mph winds
Highest sustained wind speed: 196 mph
Radius of typhoon strength winds: 53 miles
Rainfall: 400 mm
Storm surge height: 15 m
Preparation for Typhoon Haiyan
Despite being an LEDC, the Philippines take disaster preparedness seriously, as they are usually the first Pacific landmass to experience a typhoon
For decades, the Philippines have practiced risk reduction and resilience, publishing risk maps and providing evacuation shelters
The International Charter on Space and Major Disasters was triggered when Haiyan made landfall, allowing relief agencies to get satellite data from space agencies to aid recovery
The military deployed planes and helicopters in advance to areas expected to be worst hit
Community structures like conference centres were designated storm shelters, but there were concerns they would not withstand the wind
After years of community preparation and education, entire islands like Tulang Diyot were evacuated, with all 1000 residents evacuating before Haiyan
The local mayor won an award in 2011 for community work based on the 'Purok system', in which community members agree to deposit their own money into a community fund regularly for post-disaster help rather than waiting for government relief
Impacts of Haiyan
Short- and long-term impacts
Social
Short-term
6201 people died
1.1 million homes lost
more than 4 million displaced
Casualties: 28,626 from lack of aid
16 million people affected
UN admitted its response was too slow amid reports of hunger/thirst among survivors
Long-term
UN feared the possibility of the spread of disease, lack of food, water, shelter and medication
Areas less affected; an influx of refugees into the area
21,000 families were still in 380 evacuation centres two months later, waiting for the government to build bunkhouses to house them in
Economic
Short-term
Estimated at $13 billion
Major sugar/rice-producing areas were destroyed
Between 50,000 and 120,000 tonnes of sugar were lost
Over 130,000 tonnes of rice were lost
government estimated that 175,000 acres of farmland was damaged (worth $85 million)
Long-term
The Philippines declared 'a state of national calamity.’
Asked for international help the next day
President Aquino was under growing pressure to speed up the distribution of food, water, and medicine
Tacloban city was destroyed
Debt is a major obstacle for the Philippines; the country is locked in a debt cycle, with more than 20% of government revenue spent on foreign debt repayments
Environmental
Short-term
Loss of forests and trees, and widespread flooding
Oil and sewage leak into local ecosystems
Lack of sanitation in the days following led to a higher level of pollution
Coconut plantations were said to be 'completely flattened' (coconut equated to nearly half of the Philippine's agricultural exports and is the world's biggest producer of coconut oil)
Fishing communities were severely affected
Long-term
Small-scale farmers make up 90% of typhoon-affected rural populations
After 33 million coconut trees were cut, international help was sought to mill the 15 million tonnes of rotting lumber that attracted pests that threatened healthy trees
Families lack funding for local marketplaces without crops
Immediate relief
The survivors immediately searched flattened buildings for bodies
People began looting to find food supplies when the government was slow to respond
Roads were undamaged, but debris slowed rescue vehicles
Emergency teams were slowed as airports and harbours were closed, which hampered aid distribution
Diggers, land rovers, and heavy lifting gear from the UK and USA were sent to Tacloban airport by international charities
The European Commission released $4m in emergency funds and the UK Rapid Response Facility provided $8m in aid
Twelve IFRC (International Federation of the Red Cross) Emergency Response Units worldwide were deployed
The Philippines had already experienced a 7.3-magnitude earthquake in October 2013 and Typhoon Bopha in 2012. These tragedies left the Philippines short on financial, material, and human resources
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