Primary: Volcanic bombs and heat clouds, with temperatures up to 800°C, spread over a distance of 10 km
Secondary: Ash clouds caused major disruption to aviation across the region
Long-term effects of Mt Merapi eruption
Positive: 210 evacuation centres were set up in schools, churches, stadiums and government offices
Negative: -
Holderness coast
Europe's fastest eroding coast
Medium prediction for sea level rise is 30 cm in the next 50 years
Spurn Head
5km long spit that grows 10cmyearly
Protected as an SSSI
Made of boulder clay and chalk, easily erodible material
Threatened by powerful destructive waves from long fetch + winter stormsurges
Withernsea
Straight sea wall built in 1875, collapsed over time
Replaced by a curved sea wall in the 1990s at a cost of £6.3 million, £5000 per metre
Negative impacts: Waves are noisier, promenade is smaller, view from seafront is restricted, rock armour is considered ugly
Hornsea
Concrete sea wall
Groynes repaired and built at a cost of £5.2m
Rock armour
Rapid wave attacks have eroded the beach by 4m per year since the 1990s
Mappleton
£2.9 million of damage a year before management was put in place
450 metres of sea defences including rock groynes, rock armour costing £2million, and cliff stabilisation
Positive impacts: Waves no longer reach the base of the cliffs, cliff stabilisation has managed threats of mass movement, B1242 road is safe
Negative impacts: Not visually appealing, expensive, restricted access to beach, terminal groyne syndrome and sediment starvation 3km downdrift
Easington
Scheme protects gas terminal, not the village
Rock armour costing £4.5million, groynes, revetments
Why does Holderness need to be protected? (Social, economic, environmental)
Why is the erosion so bad on the Holderness coast?
Lulworth Cove
Formed after an Ice Age, where a river running to sea became swollen with glacier meltwater
Erosion of the river banks and marine erosion at the mouth widens the river
Now the sea can access soft rock behind the cliff face, and erosion accelerates to form a cove
Old Harry Rocks
Chalk formations of stack and stump
Created by hydraulic action
Chemical weathering and erosion are wearing them down
Biological weathering caused by the vegetation on the top of the headland is also breaking up the rock
Kiribati
The main island, South Tarawa, has a population of over 50,000
Most areas are under 1m below sea level
No current coastalprotection
Sea levels are rising by 12mm, 4 times higher than global average
Most places are predicted to disappear below sea levels in the next 50 years
Rising sea levels results in salinization → contamination
Shift in weather patterns could push South Tarawa into the hurricane belt
Mitigation strategies for Kiribati
Encouraging people to grow and eat local foods so migration from other islands to South Tarawa is limited
President purchased 20mh of land in Fiji for agriculture and fish farming projects
Options available to residents of Kiribati
Mitigation with dignity policy → people are allowed to apply for jobs in neighbouring countries
People can move as environmental refugees
Players in international decision making for Kiribati
IPCC, UN, USA, EU, China, Australia, New Zealand
Players' Involvement
Paris climate agreement
Carbon reduction targets
Compensation/aid
New Zealand and Australia have relocation schemes for migrants affected by climate change
Australia sends sand to replenish eroded beaches
Reason for players' involvement in Kiribati
Bangladesh
Very densely populated: population of 169 million
46% of population lives less than 10m above sea level
Will see an 11% loss of land to sea level rise alone
Sunk by 1.5 metres in 50 years
Water desalination and agriculture are at risk of sea water contamination
Fishing jobs account for 3.8% of the GDP of the country and are the most affected by sea level rise
Human factors exacerbating the situation in Bangladesh
Subsidence: Clearing and drainage of more than 50 large islands in the River delta, deforested for the growing population
Removing vegetation: Half of all global mangroves have been removed, mangroves are a natural flood defence and 71% of Bangladesh's mangrove forested coastline is retreating by as much as 200 metres per year
In the 1960s-70s large embankments were created to protect these areas but this has stopped natural deposition
Physical factors exacerbating the situation in Bangladesh
Bangladesh is on the floodplains of three major rivers – the Brahmaputra, Meghna and Ganges which converge at Bangladesh
Ice melt from the Himalayas causes flooding
Odisha, Integrated Coastal Zone Management (ICZM)
Aim: Establish sustainable economic and social activity, resolve challenges and conflict, protect coastal environment
Stakeholders: Water Resource Department, Greenspace India, Odisha Tourism Development Corporation
Issues identified: Coastal erosion and processes, vulnerability to disaster - cyclones, pollution and environmental quality management, biodiversity conservation
Flood defence in Bangladesh
71% of Bangladesh's mangrove forested coastline is retreating by as much as 200 metres per year
Caused by erosion and rising sea level
Flood defence in Bangladesh
1. In the 1960s-70s large embankments were created to protect these areas
2. This has stopped natural deposition
Physical factors exacerbating the flood situation in Bangladesh
Bangladesh is on the floodplains of three major rivers – the Brahmaputra, Meghna and Ganges which converge at Bangladesh
Ice melt from the Himalayas causes flooding
Integrated Coastal Zone Management (ICZM) in Odisha
Aim is to establish sustainable economic and social activity, resolve challenges and conflict, and protect the coastal environment
Stakeholders in Odisha's ICZM
Water Resource Department
Greenspace India
Odisha Tourism Development Corporation
Issues identified in Odisha's ICZM
Coastal erosion and processes
Vulnerability to disaster - cyclones
Pollution and environmental quality management
Biodiversity Conservation
Stakeholders in Odisha's ICZM
Residents and local community
Local government
Fishing community
Odisha Tourism Development Corp.
Ecologists and wildlife specialists
Odisha State Pollution Control Board
Cyclone Sidr
Category 4 storm that caused storm surges, high winds, and flooding in Bangladesh in 2007
Cyclone Sidr struck the Bay of Bengal
15 November 2007
Cyclone Sidr
Wind Speeds: 223 km/hr
Storm Surge Height: 4.5m-6.0m
Initial Death toll: 3363+ (rose to 1000+)
Cause: Change in sea level caused by depressions and tropical cyclones
Impacts of Cyclone Sidr
Social impacts: 1.5 million damaged houses
Economic impacts: $1.7b damage
Environmental impacts: Fresh water contamination
Nepal Earthquake
25 April 2015
Nepal Earthquake 2015
Magnitude: 7.8
Depth: 15km, Shallow
Cause: Indian and Eurasian plate destructive collision boundary
Epicentre was close to Nepal's capital Kathmandu (80km from capital)
Impacts of Nepal Earthquake 2015
Social impacts: 9,000 people died, 21,000 were injured, 3 million were displaced
Economic impacts: More than half a million houses collapsed or were seriously damaged, Infrastructure was destroyed, Damage to agricultural land, Decrease in tourism, Loss of US$5 billion from Nepal's economy (about 25% of Nepal's GDP)
Physical factors that exacerbated the Nepal Earthquake
Earthquake was shallow – depth of 15km
Epicentre was close to Nepal's capital Kathmandu (80km from capital)
The Himalayas is geologically young meaning more landslides
Nepal is mountainous and a multiple hazard zone, triggering landslides
Many large aftershocks caused further damage and deaths
Human factors that exacerbated the Nepal Earthquake
The local earthquake science is out of date
High population density in Kathmandu – 13,000 per km2
Nepal has a poor (vulnerable) population
Many homes are owner-built and do not follow building codes
Nepal has weak infrastructure – roads, bridges and safe water supplies
The emergency services were unable to cope
There is a low population density in rural areas which is where the worst damage occurred from the Nepal Earthquake