Give the concentration of atmospheric carbon dioxide before industrialisation and today.

About 280 parts per million before industrialisation, and more than 420 parts per million today.

Explain how carbon dioxide alters the Earth's energy budget.

It lets incoming short-wave solar radiation pass through but absorbs outgoing long-wave radiation from the surface and re-radiates part of it downwards, so less heat escapes to space and the lower atmosphere warms.

What is meant by radiative forcing?

Radiative forcing is the change in the balance between incoming and outgoing radiation caused by a factor such as rising greenhouse gases, measured in watts per square metre.

Why does a warmer atmosphere hold more water vapour?

The amount of vapour air can hold before saturating rises with temperature, so warmer air carries more moisture.

Explain how warming intensifies the water cycle.

Higher temperatures raise evaporation and allow the air to carry more moisture, so evaporation and precipitation both increase and water is moved through the cycle faster.

WJEC A-Level Geography 601-8455-3

Coastal Landscapes

Glaciated Landscapes

Topic overview The glacier as an open system Climate change and the glacier budget Glacier movement Types of ice mass and their distribution Glacial weathering and erosion processes Macro-scale erosional landforms Glacial transport and depositional landforms Fluvioglacial landforms Suites of landforms in glacial landscapes Periglacial processes and ground ice Periglacial action of water and wind Glacial change over different timescales Glacial environments and human activity

Tectonic Hazards

Topic overview The internal structure of the Earth Mechanisms of plate movement Divergent and conservative plate margins Convergent margins and subduction Hot spots and the global distribution of tectonic hazards The hazard profile and measuring magnitude Types of volcano and styles of eruption Primary volcanic hazards Secondary volcanic hazards Impacts of volcanic activity at different scales Contrasting volcanic eruptions Earthquake characteristics and seismic waves Earthquake hazards and ground behaviour Tsunami processes and impacts Contrasting earthquake events Risk, vulnerability and human factors Monitoring, prediction and warning Mitigation, response and the hazard management cycle

Changing Places

Topic overview What gives a place its character Flows and connections that shape places Meaning, perception and attachment to place How places are represented Economic restructuring and the Clark Fisher model Deindustrialisation and social inequality The service economy and its impacts The knowledge economy and clusters Rebranding rural places Managing change in rural places Rebranding urban places Managing change in urban places Comparing a home place with a contrasting place How place change affects people's lives

Water and Carbon Cycles

Topic overview The water cycle as a global system and mass balance Global water stores and residence times Cryospheric processes and sea-level change Drainage basin inputs, stores and outputs Flows within the drainage basin River regimes and their controls Storm hydrographs and hydrograph shape Air uplift, cloud formation and precipitation Excess runoff and flooding Deficit in the water cycle and aquifer recharge The global carbon cycle and its stores Carbon pathways between land and the atmosphere Carbon transfers involving the oceans Carbon stores in biomes and land-use change Changing carbon stores in peatlands Rising atmospheric carbon and its impacts Feedback within and between the water and carbon cycles

Global Migration

Topic overview Globalisation and a shrinking world Classifying and mapping migration Causes of international economic migration Consequences and management of economic migration Refugee movements and internal displacement Rural-urban migration in developing countries Superpowers and global hub cities Migration policy and public debate in the UK Managing refugee crises Informal settlements in developing cities

Global Governance of the Oceans

Topic overview Supranational institutions and global governance Laws and agreements governing the oceans Strategic value of the oceans and maritime security Shipping, cables and illicit flows Sovereignty over ocean resources Managing marine environments Ocean pollution and its management Governance across scales: an ocean case study

EcosystemsContemporary theme

Topic overview The value of ecosystems to people The distribution of global biomes Ecosystem structure, energy flow and productivity Nutrient cycling in contrasting biomes Measuring and threatening biodiversity Conserving biodiversity Succession and local ecosystems The Arctic tundra biome Sustainable use of the Arctic tundra

Economic Growth and Challenge: IndiaContemporary theme

Topic overview India's relief, drainage and climate India's population, society and governance India's resources, hazards and economic geography India's global role and economic growth Environmental pressures of India's growth Sustainable development strategies in India

Economic Growth and Challenge: ChinaContemporary theme

Topic overview China's relief, drainage and climate China's population, society and governance China's resources, hazards and economic geography China's global role and economic growth Environmental pressures of China's growth Sustainable development strategies in China

Development in an African ContextContemporary theme

Topic overview Defining and measuring development Physical factors influencing development Economic factors influencing development Political, social and cultural factors in development The environmental cost of development Desertification Strategies to promote development

Energy Challenges and DilemmasContemporary theme

Topic overview Classifying and distributing energy resources Physical factors in energy supply The changing demand for energy Managing oil and gas globally Problems of extraction, transport and use Energy mixes and development Sustainable solutions to energy demand

Weather and ClimateContemporary theme

Topic overview Structure of the atmosphere and the heat budget Global atmospheric and oceanic circulation The world's major climate types Weather and climate of Wales and the UK Extreme weather and ENSO Hazards of low and high pressure systems Urban climates and air quality People, climate and the future

Fieldwork and Geographical Skills

Topic overview The six-stage enquiry process Sampling and data collection Presenting geographical data Statistical analysis of geographical data Fieldwork techniques and apparatus Map skills: grid references, latitude and longitude, scale and direction

Key Concepts in Geography

Topic overview Systems, equilibrium and feedback Causality, interdependence and mitigation Resilience, risk and sustainability Place, space, scale and representation

Water and Carbon Cycles

Rising atmospheric carbon and its impacts

2 things to know
A2 Unit 3

Overview

How carbon dioxide alters the Earth's energy budget, radiative forcing and how warming intensifies the water cycle.

What you need to know

Answer each one before you reveal it.

Your recallNot started

Key term

Give two ways in which warming alters river discharge in a snow-fed basin.

Key term

State the two main causes of the recent rise in atmospheric carbon dioxide.

Questions from this subtopic

Each one with the model answer underneath.

1
State the two main causes of the recent rise in atmospheric carbon dioxide.
Model answer
The combustion of fossil fuels, and changes in land use, above all deforestation.
2
Give the concentration of atmospheric carbon dioxide before industrialisation and today.
Model answer
About 280 parts per million before industrialisation, and more than 420 parts per million today.
3
Explain how carbon dioxide alters the Earth's energy budget.
Model answer
It lets incoming short-wave solar radiation pass through but absorbs outgoing long-wave radiation from the surface and re-radiates part of it downwards, so less heat escapes to space and the lower atmosphere warms.
4
What is meant by radiative forcing?
Model answer
Radiative forcing is the change in the balance between incoming and outgoing radiation caused by a factor such as rising greenhouse gases, measured in watts per square metre.
5
Why does a warmer atmosphere hold more water vapour?
Model answer
The amount of vapour air can hold before saturating rises with temperature, so warmer air carries more moisture.
6
Explain how warming intensifies the water cycle.
Model answer
Higher temperatures raise evaporation and allow the air to carry more moisture, so evaporation and precipitation both increase and water is moved through the cycle faster.

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Coastal Landscapes

Glaciated Landscapes

Tectonic Hazards

Changing Places

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Governments must win votes.

ruralurbanelite

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AFew coastal people recognised the signs.

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The Mariana Trench reaches almost 11,000 m below sea level.

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