Studied by 2 people
Finished knowt with entire Hazards spec completed- EXAMPLES IN GREEN (examples not case studies), STATISTICS IN RED HIGHLIGHT
What is a natural hazard?
A natural event (for example earthquake, volcanic eruption, tropical storm, flood) that threatens people or has the potential to cause damage, destruction and death. An event needs the interaction of people to make it a hazard.
What is an atmospheric hazard?
Hazards that form due to influences in the atmosphere, by the movement of air and water.
What are Geomorphological hazards?
Hazards that occur on the earth’s surface.
What are tectonic hazards?
Hazards that form due to the movement of tectonic plates in the earth’s crust.
What are biological hazards?
Any biological substance that poses a threat to the health of people, e.g. viruses
Explain how level of development affects hazard risk
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.
Explain how frequency of hazards affects hazard risk
The more often a hazard occurs, the more likely people are prepared, which leads to less deaths as people know how to stay safe during the disaster.
Infrastructure and lifestyles can be adapted in areas of high frequency, lowering risk of damage.
Emergency services are also more likely to be prepared for hazards in high frequency areas, reducing death risks.
What is a plate boundary?
The boundary or margin between two tectonic plates
Describe the internal structure of the Earth
Inner core- solid
Outer core- liquid
Mantle- Molten liquid
Crust- Solid
What are the two types of crust? Describe the difference between them.
Oceanic crust (under oceans)- thinner, heavier and denser, newer material
Continental crust (under land)- thicker, lighter and older material
(oceanic crust is like a thin sheet of metal, while continental crust is a big block of cardboard)
Describe how convection currents move tectonic plates
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.
Describe how ridge push and slab pull move tectonic plates
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.
Describe the global distribution of earthquakes and volcanic eruptions and their relationship to plate margins
Patterns in the distribution of earthquakes and volcanoes match where plate margins are located.
The large band of volcanoes and earthquakes which circles the pacific ocean is known as the Ring of Fire.
Earthquakes and volcanoes can occur in the middle of plates too, in areas known as hot spots.
For example, Hawaii is located on a hot spot far from the edge of the Pacific plate.
What is the focus of an earthquake?
The point where the pressure is released within the earth’s crust.
What is the epicentre of an earthquake?
The point on the earth’s surface directly above the focus.
What are seismic waves in an earthquake?
Shockwaves that spread out from the focus of an earthquake.
How does the distance from the focus affect the strength of seismic waves?
The further away from the focus, the lower the strength of the waves.
The closer to the earth’s surface the focus is, the stronger the seismic waves will be.
If the focus is lower down in the crust, the shockwaves will be less powerful and would have less of an impact.
Describe how plates move at constructive plate margins. Give an example of a constructive plate boundary.
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.
Describe how constructive plate movement leads to earthquakes and volcanic activity.
Constructive plate margins lead to gentle volcanoes where the magma erups onto the surface, forming a volcano with gentle slopes.
Earthquakes are caused by the movement of magma through the crust.
Describe how plates move at destructive plate margins. Give an example of a destructive plate boundary.
Two plates move towards each other and collide.
If two continental plates collide, they are both light and cannot sink into the mantle. Compression forces the plates to collide and form fold mountains.
If an oceanic and continental plate collide, the denser oceanic plate is subducted under the continental plate as the oceanic crust is thinner and heavier.
Example- Nazca plate collides with the South American plate
Describe how destructive plate movement leads to earthquakes and volcanic activity.
As the oceanic plate is subducted under the continental plate, the oceanic crust melts due to heat in the mantle. Hot magma rises through gaps in the crust, causing explosive volcanoes.
When the two plates converge, friction and pressure builds as the crusts scrape against each other. The rocks eventually fracture and release pressure, causing an earthquake.
Describe how plates move at conservative plate margins. Give an example of a conservative plate boundary.
Two plates slide parallel to each other. This can be in the same direction at different speeds or in the opposite direction to each other. It doesn’t matter. Nor does it matter whether they are oceanic or continental crust.
Example- San Andreas Fault, USA.
North American plate and Pacific plate slide past each other.
Describe how conservative plate movement leads to earthquakes and volcanic activity.
As plates slide, friction and pressure builds. This pressure is suddenly released, causing an earthquake.
Volcanoes are not formed at conservative plate margins. Magma cannot rise as there is no gap created between the tectonic plates, nor any plate being subducted into the mantle.
What is the definition of a primary effect of a tectonic hazard?
The immediate damage caused as a direct result of a tectonic hazard, e.g. deaths, destruction of buildings
What is the definition of a secondary effect of a tectonic hazard?
Consequences of tectonic hazards that occur later and indirectly as a result of the initial disaster, e.g. reduced tourism, aftershocks.
Introduce the L’aquila earthquake with its location and magnitude. (HIC case study)
Give 4 primary effects of the earthquake
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
Give 4 secondary effects of the HIC L’aquila earthquake
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
What were the immediate and long term responses to the HIC L’aquila earthquake?
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
Introduce the Gorkha earthquake with its location and magnitude. (LIC case study)
Give 4 primary effects of 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
What are the secondary effects of the LIC Gorkha earthquake?
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
What were the immediate and long term responses to the LIC Gorkha earthquake?
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
Name factors that affect hazard risk and why
These factors explain the varying effects and responses between the LIC Gorkha and HIC L’aquila earthquake
Medical facilities- The more medical resources, the easier for victims to get treatment.
Transport infrastructure- The better the transport network, the quicker it is to evacuate and for aid to arrive
Population density- The more people, the more potential for risk of injuries and fatalities
Construction standards- Buildings with strict regulations are more secure and have less chance of collapsing
Distance from epicentre- The closeer to the epicentre, the greater the magnitude will be
Time and day- Buildings and roads that collapse when they are empty reduce casualties, e.g. more schoolchildren would have died if a school collapses on a weekday
Resources and finance- The more resources and money available, the quicker it is to rebuild homes and hospitals
Why do people continue to live in areas at risk from a tectonic hazard? Give 5 reasons.
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
What is monitoring/prediction?
Recording physical changes, e.g. earthquake tremors, to forecase when and where a natural hazard might strike
What is protection?
Actions taken before a hazard strikes to reduce its impact, e.g. educating people or improving building design
What is planning?
Preparing actions during and recovering from a disaster, enabling communities and authorities to act quickly and without chaos, e.g. emergency evacuation plans
Give 4 ways that show how technology is used to monitor and predict earthquakes and volcanoes to reduce the risks of a hazard
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
Give 3 ways that show how planning actions during and after earthquakes and volcanoes reduces the risks of a hazard
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
Give 2 ways that show how protection from earthquakes and volcanoes reduces the risks of a hazard
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
What does the term ‘insolation’ mean?
Exposure to the sun’s rays; the amount of solar radiation reaching a given area on the earth’s surface
What is the Global Atmospheric Circulation model?
A worldwide system of winds moving heat FROM the equator TO the poles in order to reach a balance in temperature.
Explain wind formation
Winds are large scale movements of air due to differences in air pressure.
Air always moves from high pressure to low pressure, and this movement of air generates wind.
This pressure difference is because the sun heats the earth’s surface unevenly. Insolation at the equator is greater than the insolation at the poles due to the angle of the earth’s tilt.
Why do pressure cells form?
Hot air rises and cool air sinks through the process of convection.
The irregular heating of the earth’s surface creates pressure cells, each generating different weather patterns.
What is the 3-cell atmospheric wind model? Why does the earth need it?
Each hemisphere has three cells (the Hadley cell, Ferrel cell, and Polar cell) which circulates air from the surface through the atmosphere and back.
The air redistributes energy around the world so that the equator and poles are habitable and not recieving/losing too much heat.
Hot air (rises/falls)
Cold air (rises/falls)
Low pressure areas due to (hot/cold) (rising/sinking) air
High pressure areas due to (hot/cold)
(rising/sinking) air
Low pressure = (low/high) rainfall
High pressure = (low/high) rainfall
Hot air rises
Cold air falls
Low pressure areas due to hot rising air
High pressure areas due to cold sinking air
Low pressure = thick clouds, high rainfall
High pressure = hot dry clouds, low rainfall
Describe the link between air pressure and surface winds
Surface winds move from high pressure areas to low pressure areas
Why do areas close to the Equator usually have high rainfall
High amounts of insolation near the equator, making it a low pressure zone where there is lots of rising air, forming thick clouds which rise, cool, and condensation occurs, causing lots of heavy rainfall.
Explain the circulation at the Hadley cell
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
Explain the circulation at the Ferrel cell
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
Explain the circulation at the Polar cell
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
What is the Coriolis effect?
The Coriolis effect is the appearance that the global winds and ocean currents curve as they flow, due to the Earth’s rotation on its axis, forcing the winds to blow diagonally.
In the northern hemisphere, it curves the winds to the right
In the southern hemisphere, it curves the winds to the left
What is a tropical storm?
A tropical storm is an intense destructive rotating low pressure system which forms in the tropics and results in strong winds and heavy rainfall.
What is the difference between a hurricane, cyclone and typhoon?
The tropical storm has a different name where it occurs.
In US- hurricanes
In South Asia- cyclones
In East Asia- typhoons
Describe the global distribution of tropical storms
They form in the tropics
5-20 degrees north and south of the equator
What are key factors needed for tropical storms?
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
Identify features of a tropical storm
Circular shape
Bands of swirling cloud/circling storm clouds
Eye
Eye wall
Central eye of the storm where there is no cloud
Describe the formation/cause of a tropical storm
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
How does the Coriolis effect influence tropical storms?
The Coriolis effect makes low pressure systems spin anti-clockwise in the Northern hemisphere, and clockwise in the Southern hemisphere.
What hazards are associated with tropical cyclones?
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
How does climate change affect the distribution, frequency and intensity of tropical storms?
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
Explain the distribution of tropical storms using the relationship between tropical storms and general atmospheric circulation
The global distribution of tropical storms is related to the general atmospheric circulation that transports heat from tropic to polar latitudes.
Tropical storms develop in the tropics on the low pressure zone around the Equator
once they gain energy, they can travel further away from the equator
they cannot develop directly on the equator because the Coriolis effect is not strong enough and is needed for tropical storms to spin
Explain the difference between primary and secondary effects of tropical storms
Primary effects are immediate impacts of strong winds, high rainfall and storm surges (storm surges are when the sea level rises rapidly)
Secondary effects are the impacts that occur later on after the storm has passed.
What are primary effects of tropical 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
What are secondary effects of tropical storms
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
What are immediate responses to a tropical storm?
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
What are long term responses to a tropical storm?
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
Introduce a named example of a tropical storm to show its effects and responses
Typhoon Haiyan was a category 5 storm that struck the Philippines in 2013 with wind speeds of over 315 km/h.
What are 5 primary effects of Typhoon Haiyan
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
What are 5 secondary effects of Typhoon Haiyan
Flooding caused groundwater supplies to be contaminated with sewage
increased risk of waterborne diseases such as cholera
low sanitation, pressure on damaged hospitals as less people had access to clean water
contaminated fishing waters- impact on industry, local employment and food shortages/food prices
more people fought for food, stampedes for rice supplies
What were immediate responses to Typhoon Haiyan?
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
What were long term responses to Typhoon Haiyan?
Scheme to upgrade buildings when rebuilding to defend better against future disasters
A new storm surge warning system for citizens to evacuate in time
How can monitoring and prediction reduce the effects of tropical storms?
How are tropical storms monitored?
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.
How can planning reduce the effects of tropical storms? (Planning to reduce impacts)
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
How can protection reduce the effects of tropical storms?
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
Name 6 weather hazards experienced in the UK and state the damage/ why they are a hazard
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
Introduce a recent extreme weather event in the UK to illustrate causes, impacts, and how management strategies can reduce risk
An example of a recent extreme weather event in the UK were the Somerset Levels Floods in 2014. Somerset is an area of low-lying farmland in south-west England. It had been developed for farming and residents, so many people were at high risk from the flood event.
Name one cause of the Somerset Levels Floods 2014
Very high rainfall, 100mm above average
Name 3 social impacts of the Somerset Levels Flood 2014
over 600 houses flood
residents evacuated to temporary accomodation
restricted access to flooded villages
impacting daily lives (schools, shopping)
Power supplies cut off
Name 3 economic impacts of the Somerset Levels Flood 2014
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
Name 2 environmental impacts of the Somerset Levels Flood 2014
huge amount of debris needed to be cleared
waters contaminated with sewage and chemical pollutants
Name 3 immediate responses to manage the flood to reduce risk
Emergency aid to rescue victims and treat survivors
Villagers used boats to attend school and go shopping
Local community groups gave supplies and support
Name 3 long term responses to manage the flood to reduce risk
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
What is the Quaternary period?
The last 2.6 million years where there was a global drop in temperature and a gradual cooling with warmer interglacial periods.
What is the definition of climate change vs global warming?
Climate change is a long-term change in the earth’s climate due to an increase or decrease in the average atmospheric temperature.
Global warming is the recent trend of an increase in average global temperature.
How do ice cores give evidence for climate change from the beginning of the Quaternary period to present day?
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
How do ocean sediments give evidence for climate change from the beginning of the Quaternary period to present day?
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
Why aren’t ice cores and ocean sediments reliable methods to give evidence for climate change? Suggest a more reliable method
These methods are not reliable because they only indicate climate change rather than provide direct evidence of accurate temperature.
A more reliable method would be measuring the size of ice sheets and glaciers to analyse thermal expansion and melting.
Give 4 examples of recent evidence for climate change
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
Explain how orbital changes are a natural cause of climate change
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
Explain how solar output and sunspot activity is a natural cause of climate change
The output of the sun is measured by observing sunspots on its surface. Sunspot activity dictates the heat given by the sun.
Increased sunspot activity leads to hotter temperatures,
e.g. very few sunspots were observed by satellites during colder periods
Explain how volcanic activity is a natural cause of climate change.
Explain why volcanic activity can affect global climate.
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.
Name the 4 main greenhouse gases
Carbon dioxide
Nitrous oxide
Methane
Water Vapour
What are the natural sources of the 4 main greenhouse gases
Carbon dioxide- respiration, volcanic eruptions
Nitrous oxide- soils and oceans
Methane- emitted from soils due to decomposition
Water Vapour- evaporated from oceans and plant leaves
What is the enhanced greenhouse effect?
What is the difference between the greenhouse effect and the enhanced greenhouse effect?
The impact on the climate from the additional heat retained due to the increased amounts of greenhouse gases that humans have released into the earth’s atmosphere.
The greenhouse effect is needed to make earth livable. The enhanced greenhouse effect is being caused by the incease of greenhouse gas emissions and is leading to global warming.
Explain the stages of the greenhouse effect
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
Explain the stages of the enhanced greenhouse effect
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
Explain how human’s use of fossil fuels causes climate change
Burning fossil fuels releases carbon dioxide into the atmosphere, accounting for over 50% of global greenhouse gas emissions.
Fossil fuels are used in transport, generating electricity, heating and manafacturing.
As the world’s population grows and wealth increases, people are demanding more and more energy, increasing the amount of fossil fuels burned and therefore CO2 released.
Explain how agriculture causes climate change
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.
Explain how deforestation causes 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
Give 4 social effects of climate change
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
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