Finished knowt with entire Hazards spec completed- EXAMPLES IN GREEN (examples not case studies), STATISTICS IN RED HIGHLIGHT
Determines how much money is available to prepare for the event and predict the hazard.
HICs can afford the technology to predict events and broadcast the disaster so that people can evacuate in time.
HICs can also afford better infrastructure which leads to less chance of death and damage.
HICs have better access to emergency resources and help.
Heat from the core heats material in the mantle, and causes magma to rise (hot air rises).
The magma rises towards the top of the mantle, and sinks towards the lower part of the mantle when it cools.
Magma pulls/pushes the crust when it drags along the top of the mantle and sinks back down.
This process repeats to form a convection current.
Slab pull- Destructive plate boundary
Dense oceanic crust is being PULLED by gravity into the mantle.
The oceanic plate is subducted underneath the continental plate and sinks into the mantle.
Ridge push- Constructive plate boundary
Magma rises from mantle as plates move apart and solidifies to form new land.
This new land PUSHES the crust away from the plate margin.
Two plates move apart.
Hot molten magma rises to fill the gap.
Magma cools and solifies constructing new land.
Example- Mid-Atlantic ridge
Eurasian plate moves away from the North American plate.
An example of a tectonic hazard in a high income country is the 6.3 magnitude earthquake in L’aquila Italy.
As a direct result of the earthquake, 300 people were killed. (social)
Culturally significant buildings were destroyed, including the National Museum
Social- tourism reduced
Economic- cost of damage
Hospital was damaged, patients had to be evacuated to someplace else as the damage in the hospital was too severe to treat injured victims
Social- death/injuries
Economic- cost of damage
Aftershocks triggered landslides
Economic- caused damage to housing and transport
Number of students at L’aquila university decreased
Lack of housing for residents meant house prices and rents increased
Reduced amount of business, tourism and income
Immediate responses
Electricity and Gas bills were suspended
Free mobile cells were handed to people who had lost their homes
Emergency camps were set up providing water and medical care
Ambulances and fire engines were sent in to rescue survivors
Long term responses
Free public transport and discounts on educational support for students
Historic centres were expected to take 15 years to rebuild
An investigation into why modern buildings weren’t able to withstand the earthquake
An example of a tectonic hazard in a low income country is the 7.8 magnitude earthquake in Gorkha in Nepal.
1 million were made homeless
Historic buildings and temples collapsed
Economic- reduced tourism and cost of rebuilding
50% of schools were destroyed
Social impacts on education and literacy rate in the long term
A reduction in tourism, employment and income to Nepal
Rice stored in homes was ruined in the rubble
Social- caused food shortages and income losses
2/3 of population depend on farming
Immediate responses
Emergency shelters providing medical care and water to survivors
Medical care was crucial as the earthquake was during the monsoon season, increasing the risk of waterborne diseases
Several companies did not charge for telephone calls in the days after the earthquake
Long term responses
Tourism Ministry had extended Mount Everest climbing permits to encourage people back in an attempt to boost tourism
Rebuilding of houses, roads, schools
Heritage sites reopened in time for the tourism season
Farming- Volcanic areas have very fertile soil that is rich in nutrients and good for farming
land can be farmed productively in these areas to provide a source of food and income
Mining- Valuable minerals are found in volcanically active areas
Despite being dangerous, mining provides an income
Family/Income in LICs- People in LICs cannot afford to move due to lack of transport/expensive accomodation elsewhere/cannot leave family behind
Tourism- Tourists visit volcanoes for spectacular views
100 million people visit volcanic sites every year
Tourism gives good income for local people
Preparation- Some places are well prepared for hazards so residents feel safe
Seismometers measure tremors or shocks that occur before the big earthquake
Mapping earthquake locations and times to predict when the next earthquake will occur by spotting patterns in the data
Thermal heat sensors detect changes in the temperature of a volcano’s surface
Tiltmeters measure ground deformation that signals magma collecting near the surface, predicting a volcano
Preparing emergency aid supplies so that food, water, medicine and shelter are accessed faster
Earthquake drills reducing chaos and confusion and ensuring people evacuate safely and quickly during the disaster
Exclusion zones preventing people from entering vulnerable areas near active volcanoes
Designing earthquake resistant buildings with reinforcements to prevent collapse, withstand seismic waves and minimise damage
Fire resistant materials
Shock-absorbing foundations
Shatterproof glass
Education on how to prevent futher injury and the dangers of volcanoes
Buildings cannot be designed to withstand lahars (mudflows) and lavaflows, so education on how to lookout for these dangers is the best protection
The Hadley cell extends from the equator to between 30 and 40 degrees north and south
At the equator, insolation causes air to rise, creating a low pressure zone the earth’s surface
As the air rises, it cools and sinks
The sinking air forms a subtropical high-pressure zone
The air becomes warmer and drier as it sinks, creating an area of little cloud and low rainfall where deserts are found
The air flows back towards the equator as trade winds
The Ferrel cell occurs from the edge of the Hadley cell to between 60 and 30 degrees north and south of the equator
Air on the surface is pulled towards the poles
The winds pick up moisture as they travel over the oceans
They meet cold air that has drifted from the poles
The warmer air from the tropics is lighter than the cold polar air, so the warmer air rises
This causes a low pressure zone near the surface as the warm air rises, causing unstable weather conditions and wet and windy weather
The Polar cell occurs at 60 degrees north and south
At the poles, air is cooled and sinks towards the ground, creating an zone of high pressure
It flows towards the lower latitudes
Here, the cold air mixes with the warmer tropical air and rises, creating a zone of low pressure
This causes unstable weather conditions
Warm ocean water temperatures
5-20 north and south of the equator
any closer and there is not enough spin from the rotation of the earth
the Coriolis effect causes the storm to spin, causing a rotating mass of clouds
Tropical regions- warm temperatures where insolation is high
Low pressure areas where warm air is converging and rising rapidly
Circular shape
Bands of swirling cloud/circling storm clouds
Eye
Eye wall
Central eye of the storm where there is no cloud
Hot sea temperatures cause warm air to rise quickly
This creates an intense low pressure zone
The rising air draws further warm air up from the ocean’s surface, generating stronger winds
The air spirals upwards, cools and condenses to form large clouds
The rotation of the earth on its axis sets up a spinning motion
These clouds form the eye wall of the cyclone and produce heavy rainfall and the strongest winds
In the centre of the storm, cool air sinks, creating calm and dry conditions known as the eye of the storm
The storm is carried across the ocean by the prevailing winds, picking up more moisture across the sea as it moves, becoming more powerful
Tropical storms die out when they reach land as the heat energy and moisture from the ocean are no longer available to drive the storm
Storm surges
Strong winds that can tear off roofs, break windows and damage communication and transport networks
Torrential rain and flooding- the warm humid air from cyclones produces huge amounts of rainfall and flooding as the cyclone moves inland
Frequency and Distribution
More of the world’s oceans will have higher temperatures as a result of global warming, so more places across the world will experience tropical storms.
Warmer oceans means tropical storms will affect areas further north and south of the equator
more low-lying coasts are at higher risk
Oceans will stay at high temperatures for longer during the year, increasing the frequency of tropical storms
Intensity
Higher temperatures increase the wind speed, causing storms to be stronger and cause more damage
Estimated to have a higher number of category 4 and 5 storms
High wind speeds destroy infrastructure such as electricity power lines, houses and villages and can out crops
Torrential rainfall can result in extensive widespread flooding
Amount of destruction depends on storm’s strength and how well people are prepared and protected.
Damage to houses can force people to live in temporary shelters
Lack of shelters/overcrowded shelters can cause distress, homelessness and death
Cost of rebuilding homes are expensive
Blocked or destroyed roads prevent emergency vehicles and aid from getting through
Hospitals, shops and homes won’t have a power supply
Damage to crops can cause shortage of food, increased food prices and famine
Flooding can cause drowning or injuries
Potential unemployment from economic impact and destruction of businesses and infrastructure
Warning systems broadcast information to the public
Evacuation to higher ground or emergency storm shelters away from the impacts of storm surges
Distributing emergency food and water to survivors
Repairing damge to existing buildings and infrastructure
Ensuring the country is capable of managing a future hazard by investing in methods of protection and prediction, e.g. new sea defences or a new warning system
Over 6000 people died
High wind speeds
Interrupted power supplies, damaged infrastructure, blocked roads with trees and debris
Heavy rainfall flooded 1km inland
1 million houses were destroyed- temporary shelters overcrowding, poverty and distress
Authorities evacuated 800,000 people with many seeking refuge in a stadium
Emergency aid supplies arrived once the airport was reopened
A curfew was imposed 2 days after the typhoon to stop looting
Food packs and water were distributed
Scheme to upgrade buildings when rebuilding to defend better against future disasters
A new storm surge warning system for citizens to evacuate in time
Satellites- tropical storms have an identifiable cloud pattern that satellites monitor
Wind strength can be monitored by measuring wind speed
National Weather service can announce a warning when storm winds are detected
Monitoring and Prediction alerts people and gives them time to prepare and evacuate.
Many LICs are less able to monitor and predict tropical storms as the equipment is very expensive.
Governments can plan evacuation routes to get people away from tropical storms quickly and safely
People are encouraged to stock up on food and water as they may be trapped in their homes following a storm
Training and education on the impacts of storms and how to reduce injuries during a storm
Emergency services doing storm drills
Installing warning loudspeakers
Designated emergency shelters on stilts to protect from storm surges
Buildings are less likely to collapse, less people will die from collapsing buildings and falling debris
Storm shutters on windows to reduce flying debris
Defences such as sea walls and stilted buildings to prevent damage from storm surges
Bicycles nearby to give warnings to remote communities
Lack of trees nearby buildings to reduce damage if uprooted
Protection can be expensive to put in place, but saves money in the long term as there is less need for rebuilding
Heavy rain
Risk of flooding- damage to homes, disrupts transport networks
Wind
Uprooted trees and debris can injure or kill
Thunderstorm
Can cause fires
Lightening strikes damage property and environment
May disrupt daily life if people are afraid to leave home
Hailstorm
Makes driving difficult- can damage windscreens
Can damage property and destroy crops
Drought
Insufficient water for crop production- high food prices, risk of famine
Low water reserves in resevoirs- hosepipe bans and water supply restrictions distress people
Snow/Ice
School, transport and business closures
Injury through slips and falls
Damages crops and wildlife
Disrupts transport networks
Risk of hypothermia
over 600 houses flood
residents evacuated to temporary accomodation
restricted access to flooded villages
impacting daily lives (schools, shopping)
Power supplies cut off
cost of repair estimated over £10 million
livestock evacuated from flood zone
impacting farming industry and food prices
local roads drenched in floods
impacting tourism and trade
huge amount of debris needed to be cleared
waters contaminated with sewage and chemical pollutants
Emergency aid to rescue victims and treat survivors
Villagers used boats to attend school and go shopping
Local community groups gave supplies and support
Somerset Country launched a £20 million action plan to prepare for future extreme floods
Vulnerable communities will have flood defences
Road levels are raised to maintain communication and allow business to continue during future flood events
Ice cores can be drilled to find information about the climate when the snow fell
In Antarctica there are no permanent residents, so the layers of snow remain unaltered
The layers hold information about climate change as they build up over the Quaternary period
When ice cores are melted, trapped CO2 is released, which can be compared to present levels to see the extent of climate change
Ocean sediments are sediments deposited at the bottom of the sea
Organisms and remains of plankton in the sediment reveal information such as past surface water temperatures and levels of oxygen and nutrients through the Quaternary period
The deeper the sediment, the older it is
The oxygen isotopes in ocean sediments can be used to calculate the temperature
Shrinking glaciers and melting ice
Arctic sea ice has melted by 65%
Rising sea levels
Due to rising temperatures causing meltwater from glaciers to flow to seas
Average global sea level risen by 10cm in past 100 years
Shorter hibernations
Plant flowering patterns changing
The solar radiation recieved by the earth changes depending on its orbit.
The earth’s orbit is elliptical, so as the earth orbits closer to the sun, the climate gets warmer.
The tilt of the earth’s axis changes every few thousand years. The greater the tilt, the more exaggerated the climate- hotter summers and colder winters
The earth is not a perfect sphere, so it wobbles on its axis, affecting seasonal temperatures
Violent volcanic eruptions blast huge quanities of ash, gases and liquids into the atmosphere.
Volcanic ash clouds can block out the sun, reducing temperatures on the earth as a short-term impact.
Sulphur droplets can reflect radiation and reduce solar radiation entering the earth’s atmosphere.
This is called volcanic winter.
Sun emits solar radiation
The earth absorbs most of the radiation and emits it as infrared radiation
Some infrared radiation is reflected back into space
Some infrared radiation is trapped in the earth’s atmosphere by greenhouse gases
Sun emits solar radiation
The earth absorbs most of the radiation and emits it as infrared radiation
Less of the sun’s energy is reflected back out to space as there is a bigger layer of greenhouse gases
More energy is trapped in the earth’s atmosphere by greenhouse gases, making it hotter
Agriculture accounts for over 20% of global greenhouse gas emissions.
Cattle ranching produces large amounts of methane.
Deforestation to clear land for crops leads to less CO2 being absorbed during photosynthesis.
The production of feritilisers produces fossil fuels.
Food demand is increasing with population, and rising wealth increases meet demand. Therefore, large-scale agriculture will continue to play a huge role in causing climate change.
Deforestation clears forests on a huge scale, with the destruction of these carbon sinks causing less CO2 to be absorbed during photosynthesis, and releasing CO2 when the carbon sinks are burned.
Deforestation occurs due to:
clear land for agriculture so that farmers have space to plant crops and graze livestock
logging for wood
building roads to access remote areas
making room for the expansion of urban areas
Hotter temperatures lead to heat strokes and dehydration becoming more frequent
more money spent on healthcare than improving quality of life
Fewer winter related deaths due to milder winters
Increased flooding due to sea level rise leads to displacement of huge numbers of people
More deaths related to extreme weather, e.g. more tropical storms → higher death rate