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My revision planner
Unit 1 Living with the physical environment
Section A: The challenge of natural hazards
1 Natural hazards 1 1.1 Natural hazards
2 Tectonic hazards 2 2.1 Earthquakes and volcanoes 4 2.2 Tectonic hazards 7 2.3 Management of tectonic hazards
3 Weather hazards 8 3.1 Global atmospheric circulation 9 3.2 Tropical storms 11 3.3 Effects of tropical storms 14 3.4 Weather hazards in the UK
4 Climate change 17 4.1 Causes and effects of climate change 19 4.2 Managing climate change
Section B: The living world
5 Ecosystems 20 5.1 Ecosystems
6 Tropical rainforests 26 6.1 Tropical rainforests 30 6.2 What is deforestation? 33 6.3 Management of tropical rainforests
7 Hot deserts 35 7.1 Characteristics of hot deserts 39 7.2 Case study: development of hot deserts 41 7.3 Desertification
8 Cold environments 43 8.1 Characteristics of cold environments 47 8.2 Case study: development of cold environments 49 8.3 Protection of cold environments as wilderness areas
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Sample material © Hodder Education, 2017
vAQA GCSE Geography
Section C: Physical landscapes in the UK
9 UK physical landscapes 51 9.1 UK landscapes
10 Coastal landscapes in the UK 52 10.1 Coastal processes 57 10.2 Coastal landforms 63 10.3 Coastal management strategies
11 River landscapes in the UK 67 11.1 Rivers and river valleys 69 11.2 River landforms 73 11.3 River management strategies
12 Glacial landscapes in the UK 77 12.1 Glacial processes 80 12.2 Glacial landforms 85 12.3 Land use in glaciated upland areas
Unit 2 Challenges in the human environment
Section A: Urban issues and challenges
13 Urban growth across the world 89 13.1 Global pattern of urban change 91 13.2 Case study: urban growth in Lagos 97 13.3 Case study: urban growth in Rio de Janeiro
14 Urban growth in the UK103 14.1 Urban growth in cities in the UK 106 14.2 Example: urban regeneration project in the UK
15 Urban sustainability108 15.1 Urban sustainability
Section B: The changing economic world
16 Economic development110 16.1 Measuring development 114 16.2 Uneven development
17 Strategies for reducing the development gap117 17.1 Reducing the development gap
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18 Economic development in the world119 18.1 Case study: economic development in Nigeria
19 Changing UK economy126 19.1 Economic change in the UK 128 19.2 The UK’s post-industrial economy 130 19.3 What are the impacts of industry on the physical environment? 131 19.4 Changes in the rural landscape 132 19.5 Developments in infrastructure 134 19.6 The north–south divide 136 19.7 The UK in the wider world
Section C: The challenge of resource management
20 Resource management138 20.1 The global distribution of food, energy and water
21 Resources in the UK140 21.1 Changing food demand in the UK 142 21.2 Changing water demand in the UK 144 21.3 The UK’s changing energy mix
22 Food146 22.1 Food: supply and demand 149 22.2 Food: increasing food supply 151 22.3 Sustainable food supplies
23 Water153 23.1 Water: supply and demand 156 23.2 Water: increasing supply 158 23.3 Sustainable water supplies
24 Energy160 24.1 Energy: supply and demand 164 24.2 Energy: increasing supply 167 24.3 Sustainable energy supplies
Unit 3 Geographical applications
170 Section A: Issue evaluation
171 Section B: Fieldwork
Now test yourself answers and Exam practice answers at www.hoddereducation.co.uk/myrevisionnotes
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1AQA GCSE Geography
1.1 Natural hazardsA natural hazard is a natural event such as an earthquake, volcanic eruption, tropical storm or f lood. It is caused by ‘natural’ processes, so would occur even if humans were not on the planet. However, it is a ‘hazard’ because it has the potential to cause damage, destruction and death when it interacts with humans.
What are types of natural hazard?Natural hazards are most commonly classified by the physical processes that caused them:l Earthquakes and volcanoes are classed as tectonic hazards.l Flooding is a geomorphological hazard.l Tropical storms are classed as atmospheric hazards.l Forest fires are biological hazards.
However, classifying hazards is made difficult because:l some may be caused by more than one physical process; for example, a
tsunami can be both a tectonic and a geomorphological hazardl some may also be caused or inf luenced by human processes; for
example, forest fires can be a natural biological hazard but can also be caused by human activity such as arson or falling power lines.
Factors affecting hazard riskHazard risk is the probability or chance that a natural hazard may take place. The hazard risk will increase when there is:1 an increase in the number of people vulnerable to the natural hazard;
for example: world population has increased more people are living near hazard-prone areas because they cannot move, it’s worth staying or simply they don’t want to move
2 an increase in the a) frequency (how often) and b) magnitude (strength) of the natural hazard; for example:
some hazards are more destructive than others global warming increases the probability of hazards such as f looding deforestation and urbanisation increase hazards such as landslides and f looding.
3 a decrease in the number of people capable of coping with the natural hazard; for example:
some hazards are harder to predict and it is therefore harder to evacuate people in time
some people do not have the money, knowledge or ability to cope with natural hazards when they occur. This is more likely in low income countries (LICs) than in high income countries (HICs).
1 Natural hazards
Natural event Naturalhazard
Vulnerable population
Figure 1.1 A natural hazard
Revision activity
List as many different natural hazards as you can, then colour code them to show what type of natural hazard they can be classified as.
Now test yourself1 What is hazard risk?2 List at least three factors which affect hazard risk.
Exam practice 1 Define natural
hazard. (1 mark)2 Suggest how hazard
risk would be affected by an increase in population. (2 marks)
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3.4 Weather hazards in the UK
What are weather hazards in the UK?Extreme weather is when the weather is especially severe or out of season, and is clearly different to the usual weather pattern. Most parts of the UK are at risk from one or more types of extreme weather. Different air masses crossing the UK bring a variety of weather.
0 800km
NHot and sunny weather from the south can lead to heatwaves and drought.
Severe winter weather can come from the east.
Arctic air can bring heavy snow and bitterly cold conditions.
Storms from the Atlantic bring heavy rain and strong winds.
Hot and sunny weather from the south
Severe winter weather can
Figure 3.10 Map of UK air masses
Storm eventsDepressions (low-pressure systems) bring heavy rain and strong winds to the UK, as happened in autumn 2013. Possible impacts include:l f lood and wind damage to business and propertiesl trees uprooted, causing further damagel power supplies down l disruption to transport l death.
FloodingFloods are often caused by heavy rainfall or storm waves. Torrential rainstorms and thunderstorms can cause f lash f looding. Prolonged rainfall also leads to f looding, for example as in Boscastle, 2004. Possible impacts include:l crops ruinedl damage to homes, businesses and possessionsl transport disrupted or even washed awayl death by drowningl recovery is often expensivel landslides.
Droughts and heatwavesDroughts and heatwaves are typically long periods with little or no rainfall. In the UK a drought is defined as fifteen or more consecutive days with less than 0.2 millimetres of rain on any one day, such as in summer 2003. Possible impacts include:l crop production fails and wildlife is affectedl reservoirs run low, reducing water suppliesl hosepipe bans enforcedl elderly vulnerable to heat exhaustion – possible
deathl roads can melt and railway lines can buckle.
However, the tourism industry may benefit.
Extremes of cold weatherCold conditions take over if the usual depressions (low-pressure systems) are not passing over the UK, as happened during winter 2014–15. Possible impacts include:l crops fail and cattle may not survive at –10°Cl roads, railways and airlines shutl increased injuries caused by falling in snow
and icel businesses and schools shut.
Revision activity
Practise sketching a simple map of the UK and label it with where different types of weather come from.
Now test yourself1 Describe why the UK experiences a variety of weather.2 What is extreme weather?3 Name four types of extreme weather that the UK experiences. 4 How could extreme weather affect a) agriculture b) transport
c) people’s health?5 Why might extreme weather be of benefit to the UK?
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What have been the recent extreme weather events in the UK?Both Cumbria and the Somerset Levels are examples in the UK which experienced an extreme weather event leading to widespread f looding. You are required to study one example of an extreme weather event in the UK.
Somerset Levels, UK Cumbria, UK
When December 2013 to February 2014 17–20 November 2009
Causes l Several depressions moving across the Atlantic Ocean caused weeks of wet weather.
l Saturated soil.l Wettest January on record.l High tides and storm surges came up
the rivers from the Bristol Channel.l Reduced river capacity (lots of
sediment) due to not being dredged for over twenty years.
l A month’s worth of average rainfall had fallen by 17th November.
l Saturated soil.l Steep slopes of the Lake District.l Deep Atlantic depression moving north-
eastwards over Scotland and northern England.
l Heaviest rainfall on record.
Social impacts l More than 600 homes flooded.l Sixteen farms evacuated.l Temporary accommodation for
residents needed for several months.l Some villages cut off.l Power supplies disrupted.
l More than 1,500 homes flooded.l Police officer killed when a bridge in
Workington collapsed.l Many injured.l Health risk as river water contaminated with
sewage.
Economic impacts
l Over 14,000 hectares of agricultural land flooded for weeks.
l Over 1,000 livestock evacuated.l Roads cut off.l Railway line closed.l £10 million damage estimated.
l Businesses closed, which didn’t reopen until long afterwards.
l Six important regional bridges destroyed.l £100 million damages.
Environmental impacts
l Contaminated river water with sewage, oils and chemicals.
l Large volume of debris deposited across land.
l Stagnant water had to be reoxygenated then pumped back into river.
l Landslides triggered.l Contaminated river water.l Hundreds of trees carried away, damaging
local ecosystems and habitats.
Management strategies to reduce risk
l River banks raised and strengthened.l Somerset County Council pledged £20
million on a Flood Action Plan.l Rivers Tone and Parratt were dredged
in March 2014.l Road levels raised.l Flood defences for communities at
risk.l Pumping stations built.l Potential tidal barrage at Bridgwater
by 2024.
l Central government and local community spent £4.5 million on new flood defences.
l Mobile wall built, which rises when needed but disappears from view to maintain views for tourist industry.
l Environment Agency (EA) provides residents with improved flood warning information.
l The EA sends flood warning messages directly to smartphones of Cockermouth residents.
l Adverts placed in national newspapers to publicise Cumbria was back open for business.
Now test yourself1 State three factors that caused flooding.2 Name two social, economic or environmental impacts.3 Who was involved in reducing the risk of future floods?
Revision activity
Write a series of quiz questions about the case study. Test yourself over and over until you consistently remember the answers correctly.
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Is the UK’s weather getting more extreme?Extreme weather is not new to the UK. There are many examples of extreme weather in the past. However, the frequency of extreme weather in the UK is increasing. Since the 1980s, UK temperatures have increased by about 1°C and winter rainfall has increased. There have been more weather records broken recently than ever before.
Extreme weather recordsTemperature Rainfall
l December 2010 coldest on record for 100 years. Warmest April was 2011.
l Highest temperature (38.5°C) was 10 August 2003.
l Lowest temperature (–27°C) was in Scotland in 1995.
l Highest two-day record of rainfall (405 millimetres) was in 2015.
l Highest three- and four-day rainfall records were both in 2009.
l Highest monthly total of rainfall (1,396.4 millimetres) was in 2015.
l Serious flooding has become more frequent in the winter, for example in Cumbria 2009 and the Somerset Levels 2013–14.
What are the predictions for future UK weather?l Precipitation is expected to become even more seasonal.l Some rivers are expected to f lood more frequently in winter.l Air temperature is expected to increase, causing more drought.
Is climate change responsible?Climate change cannot be responsible for individual extreme weather events. Yet scientists suggest that the increasing frequency of extreme weather events can be blamed on climate change. Evidence suggests that climate change is warming the planet. The Atlantic Ocean is increasing in temperature. This can explain the UK’s changing rainfall pattern. Rain-bearing depressions will gain more energy and moisture, due to the warmer ocean. The frequency of rain-bearing storms has increased in line with climate change predictions since the 1980s.
Research also shows that the Atlantic Ocean was relatively warm between 1931 and 1960, before cooling from 1961 and 1990, that and then warming again. The increase in ocean temperature may simply be a long-term cycle or due to the position of the jet stream and not due to climate change.
Now test yourself1 What has happened to the frequency of extreme weather events in
the UK?2 By how much have temperatures increased since the 1980s?3 Name two examples of UK weather records that have been broken
since 2000.4 Describe how a) precipitation, b) flooding, and c) air temperature
are expected to change in the future.5 Give one reason why climate change is not responsible for the UK’s
extreme weather.
Exam practice1 Give one piece of evidence
that suggests the UK’s weather is becoming more extreme. (1 mark)
2 Suggest why the UK’s extreme weather events might be increasing. (4 marks)
3 Discuss to what extent climate change is responsible for extreme weather in the UK. (6 marks)
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10.1 Coastal processesWhat are the main wave types and their characteristics?Waves are formed by the wind blowing over the sea. Friction with the water’s surface causes ripples to form, which can then develop into waves. The energy of the waves is determined by:l the strength of the windl the duration of the windl the distance of open water over which the wind blows – this is called
the fetch.
In the open water, waves have a circular (orbital) motion. As the waves approach the shore, this orbital motion is interrupted by the shallowing seaf loor, causing the waves to rise up and eventually break on the beach (Figure 10.1).
The wave breaks and flows onto the beach as swash, and gravity takes it back down the beach as backwash
In deep water, each water molecule within a wave moves in a circular motion
As waves move into shallow water, they begin to stack up
As frictional drag with the sea bed increases, the base of the wave is slowed down so the top part is travelling faster. This causes the wave to tilt, break and move towards the shore in the surf zone
Waves slow down due to friction with the sea bed, and begin to increase in height
Water molecules are now moving in an elliptical (rugby ball) shape
To the shore
Sea bed
Beach
Backwash – theretreat of a waveback towards the sea
Swash – the forwardmovement of water
up a beach as awave breaks
Figure 10.1 Waves approaching the coast
Now test yourself1 What causes waves to form?2 What happens to waves as they approach the shore?
10 Coastal landscapes in the UK
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Constructive and destructive wavesIt is possible to identify two types of wave breaking at the coast: constructive (Figure 10.2) and destructive (Figure 10.3).l Constructive waves – these are low waves with long wavelengths
formed by distant storms. On breaking, they surge up the beach with a strong swash. Water soaks into the beach, resulting in a weak backwash. Over time, they build up a beach, hence the term ‘constructive’.
l Destructive waves – these are higher waves with shorter wavelengths formed by local storms. As they crash down (plunge) onto the beach, there is little forward movement of water (swash) but powerful backwash. Over time, this results in the lower beach being eroded.
Wave types vary throughout the year, with constructive waves being more common in the summer and destructive being more common in the winter, when frequent storms approach the UK. This explains why beaches vary in their profiles and material during the course of the year.
The strong swash transports sand and shingle up the beach to construct it
Long wavelength so low frequency(8–10 waves per minute)
Low energy
Very weak backwash
Strong swash
Gains a little height, breaks and spills onto the beach Water spreads a
long way up thegently sloping beach
Wave front isgently sloping
Low wave height (under 1 metre)
Figure 10.2 Constructive waves
Gains much height
Very strong backwash
High energy
Short wavelength so high frequency at 10–14 waves per minute
Restricted swash
Plunges on to asteep beach sodoes not travelfar up the beach
Steep wave front
Wave height ofover 1 metre
The relatively stronger backwash drags beach material out to sea
Figure 10.3 Destructive waves
Revision activity
Draw simple diagrams to identify the characteristics of constructive and destructive waves.
Now test yourself1 Name two characteristics of constructive waves.2 Name two characteristics of destructive waves.
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