Coastal Management (Cambridge (CIE) O Level Geography)
Revision Note
Written by: Jacque Cartwright
Reviewed by: Bridgette Barrett
Managing the Impacts of Coastal Erosion
There are conflicting views about using a particular type of engineering 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 to be a more sustainable approach to coastal protection
However, they are not as effective as hard engineering methods
Soft Engineered Defences
Strategy | Description | Advantages | Disadvantages |
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Beach replenishment |
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Widens beach front | Has 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 |
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Cliff re-grading |
| Prevents sudden loss of large sections of cliff Regrading can also slow down wave cut notching at base of cliffs as wave energy is slowed |
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Managed retreat |
| No expensive construction costs Creates new habitats such as salt marshes | Disruptive to people where land and homes are lost Cost of relocation can be expensive Compensation to people and businesses may not be paid |
Hard engineering methods
Hard engineering involves building some form of sea defence, usually from concrete, wood or rock
Structures are expensive to build and need to be maintained
Defences work against the power of the waves
Each type of defence has its strengths and weaknesses
Protecting one area can impact regions further along the coast, which results in faster erosion and flooding
Hard engineering is used when settlements and expensive installations (power stations etc) are at risk - the economic benefit is greater than the costs to build
Hard Engineered Defences
Strategy | Description | Advantages | Disadvantages |
---|---|---|---|
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| Very expensive to build and maintain
Restricts access to the beach Unsightly to look at |
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Creates wider beaches | Stops material moving down the coast where the material may have been building up and protecting the base of a cliff elsewhere Starves other beaches of sand. Wood groynes need maintenance to prevent wood rot Makes walking along the shoreline difficult |
| Large boulders are piled up to protect a stretch of coast | Cheaper method of construction Works to absorb wave energy from the base of cliffs and sea walls |
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| Cheapest form of coastal defence
Can be stacked at the base of a sea wall or cliffs | Wire cages can break, and they need to be securely tied down Not as efficient as other coastal defences |
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| Work to break the force of the waves 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 | Not effective in stormy conditions Can make beach inaccessible for people Regular maintenance is necessary Visually unattractive |
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| Effective at breaking wave energy before reaching the shore Beach material is built up Low maintenance Maintains natural beach appearance |
Can be removed in heavy storms Can be unattractive
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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 will 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 allow for forecasting and tracking potential hazard events i.e.
Tropical storms - track the storm's path and associated storm surge
Earthquakes - size and position if underwater and possible tsunami outcome
Both these methods of forecasting help officials to say when and where the event will occur
It indicates the possible strength and scale of the flooding, and the likelihood of damage and death
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
Planning any new development away from high-risk-areas
Designing buildings to cope with low levels of flooding
Elevating buildings so that flood waters can pass underneath
Flood proof buildings with raised foundations (fixed or mechanical)
Reinforced barriers
Dry flood proofing - sealing a property so that floodwater cannot enter
Wet flood proofing - allows some flooding of the building
Buffer zones
Areas of land are allowed to flood before reaching settlements
This allows the energy in the surge to dissipate slowing down the distance the floodwater will travel
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
Identification allows resources to be allocated effectively to reduce the impacts of these risks
The 'cost to benefit' is easier to calculate using coastal cells
Shoreline management plans
Shoreline Management Plans (SMP) set out an approach to managing a coastline from flooding and erosional risk
The plans aim to reduce the risk to people, settlements, agricultural land and natural environments (salt marshes etc.)
There are four approaches available for coastal management, with differing costs and consequences:
Hold the line
Long term approach and the most costly
Build and maintain coastal defences so the current position of the shoreline remains the same
Hard engineering is the most dominant method used with soft engineering used to support
Advance the line
Build new defences to extend the existing shoreline
Involves land reclamation
Hard and soft engineering is used
Managed realignment
Coastline is allowed to move naturally
Processes are monitored and directed when and where necessary
Most natural approach to coastal defence
Mostly soft engineering with some hard engineering to support
Do nothing
Cheapest method, but most controversial of the options
The coast is allowed to erode and retreat landward
No investment is made in protecting the coastline or defending against flooding, regardless of any previous intervention
Decisions about which approach to apply 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 - local campaigns to protect the region
Social value of communities - long-standing, historic communities
Worked Example
Explain how gabions protect the coast
[2 marks]
The command word here is 'explain', therefore, there needs to be development of the answer for the full marks
Examples include:
Gabions absorb/dissipates/reduces the wave's energy/power, [1] and this reduces the impact of the waves at the foot of cliffs and seawalls, which reduces/prevents coastal erosion [1]
Case Study - Super Typhoon Haiyan
Background
Typhoon Haiyan (locally called Yolanda) was one of the strongest ever-recorded tropical storm to hit the Philippines
It made landfall on the 8th of November 2013 as a Category 5, with sustained winds of over 195 mph (315 km/hr)
The Philippines are a series of islands located in the South China Sea, east of Vietnam and north of Indonesia
The islands regularly suffer from typhoons that sweep in from the southwest every year during the tropical storm season
The islands sit in an area of usually warm ocean water, however, at time of storm, the sea temperature was 30°C
Sea level rise (since 1900, has increased 20cm around the world) is a factor as higher seas are known to contribute to greater storm surges
Abstracting too much 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) and sufficient spin from the earth’s rotation (Coriolis force), hence why they form between 5-20° N and S of the equator
Warm water encourages evaporation from the sea surface, and as the air rises, it cools, condenses, releases latent heat and forms large thunderclouds
Heat from below causes further vertical growth and this creates an intense low pressure
Tropical storms begin with a merging of several storms on 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 westwards
Winds rotate around a central eye, where cold air descends creating an area of calm
The strongest winds are within the wall of the eye.
Typhoon Haiyan's timeline
Path of Typhoon Haiyan November 2013
Date - Nov 2013 | Development |
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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 | Classified as a typhoon and a low-level Public Storm Warning is issued by Philippines Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) |
6th | Declared a Category 5 super typhoon by the Joint Typhoon Warning Center. 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
The Philippines, despite being an LEDC, take disaster preparations seriously as they have experience of typhoon impacts, as they are usually the first Pacific landmass in a typhoon's track
The Philippines have been practicing risk reduction and resilience for decades and have published risk maps and provided evacuation shelters
When Haiyan made first landfall, the International Charter on Space and Major Disasters was activated, this allowed relief agencies, in times of disasters, to have access to satellite data from space agencies to help in relief and recovery
The military deployed planes and helicopters in advance to areas expected to be worst hit
Community buildings, such as convention centres, were designated as storm shelters, but there were concerns that they would not withstand the wind
As a result of years of community preparedness and education, there were evacuations of whole islands, such as Tulang Diyot, with all 1000 residents leaving ahead of Haiyan
The local mayor won an award in 2011 for community work based on the “Purok system”, which is where community members agree to deposit their own money into a community fund, on a regular basis, for post-disaster assistance, rather than waiting for government aid
Impacts of Haiyan
Total economic loss | $13 billion |
Homes damaged or destroyed | 1.1 million |
Displaced people | 4 million |
Number of deaths | 6201 |
Number of people missing | 1785 |
Number of injured people | 28,626 |
Number of people affected | 16 million |
Impacts | Short-term | Long-term |
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Social |
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Economic |
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Environmental |
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Immediate relief
The immediate response was from the survivors, who searched flattened buildings for bodies
The government was criticised for being slow in its response, and people began looting to find food supplies
Roads were undamaged, but debris slowed rescue vehicles
Airports and harbours were closed meaning emergency teams had to travel slowly on foot, which hampered aid distribution
International charities sent emergency supplies, centred on Tacloban airport with the UK and USA sending diggers, land rovers and heavy lifting gear
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 was also dealing with two prior natural disasters - 7.3 magnitude earthquake a month earlier (October 2013) and Typhoon Bopha in 2012. Together these disasters meant that the Philippines were low on resources - financial, material and human
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