8.1.5
Burning Fossil Fuels
Fossil Fuel Combustion
Fossil Fuel Combustion
Fossil fuels are the term given to oil, coal and natural gas. All can be used as independent fuel sources or to generate electricity.
When are they combusted?
When are they combusted?
- Oil in the form of petrol is combusted (burned) in cars.
- Natural gas can be used to heat our stoves when cooking.
- All types of fossil fuel combustion release CO2 as a by-product.
Balance
Balance
- The carbon cycle is said to be in equilibrium (balance) between its stores and sinks.
- Since Industrialisation (1800's in the UK but later in Emerging and Developing countries) the combustion of fossil fuels has increased.
- As a result, the concentration of atmospheric CO2 has also increased. This has been linked to increases in global temperatures due to enhancing the Greenhouse Effect.
Impact on climate
Impact on climate
- Globally, higher levels of atmospheric CO2 increase global temperatures. Locally, the impacts vary.
- Eastern and Northern Europe are expected to see warmer winters, whilst Southern Europe is projected to see warmer summers.
- Northern Europe is expected to see an increase in precipitation whilst Southern Europe is projected to see less precipitation.
- This will decrease water availability and increase the likelihood of drought and forest fires in Southern Europe.
Extreme weather events
Extreme weather events
- With the changes in temperature and precipitation, it is likely that extreme weather events will increase.
- E.g. the likelihood that sea surface temperature will reach 27oC for 3 consecutive weeks (a prerequisite for Tropical Storms) will increase and the area where this is possible will increase.
- Therefore, the areas hit by tropical storms will increase as will their intensity.
Impact on the Arctic
Impact on the Arctic
Whilst warming is noted globally, the Arctic is warming at twice the rate. This is known as Arctic amplification.
Effect on permafrost
Effect on permafrost
- Warmer temperatures in the Arctic cause more permafrost to thaw, which releases the stored CO2 and CH4 (Methane).
- This leads to more greenhouse gases, impacting the greenhouse effect, rising global temperatures and causing more permafrost to thaw.
- Some studies now show that the carbon may remain in new vegetation that is able to grow now the permafrost has thawed. This new plant growth may allow carbon to be stored via photosynthesis.
Snow and ice changes
Snow and ice changes
- Sea ice melts and snow cover is reduced with increasing temperatures.
- This reduces the albedo effect, allowing more solar radiation to be absorbed by the earth and resulting in an even greater increase in temperature.
- The change in habitat is devastating for the ecosystem dependent on it.
- E.g. The native Arctic Fox now must compete for food and territory with the red fox (from Alaska), which has migrated North into now habitable land.
Impact on the Hydrological Cycle
Impact on the Hydrological Cycle
Precipitation rates and the effects of glacial melt are expected to change with global warming. This will result in changes to river discharges and flooding.
Precipitation
Precipitation
- If precipitation falls as rain and not snow in winter, winter floods can be expected.
- Summer droughts and forest fires will be increasingly common.
Glacial meltwater
Glacial meltwater
- As glaciers retreat (melt more than they form each year) there will be an increase in river discharge and sediment yields until glaciers have completely gone.
- Currently, European countries receive water during the summer months from Alpine glacial meltwater.
- Studies show limited ice in the Western Alps and none in the Eastern Alps by 2100.
- This will have knock-on impacts on river discharge.
1Tectonic Processes & Hazards
1.1Tectonic Processes & Hazards
1.2Natural Disasters
1.3Natural Disaster Case Studies
1.4Trends & Patterns
2Option 2A: Glaciated Landscapes & Change
2.1Glaciated Landscapes Over Time
2.2Periglacial Landscapes
2.3Glacial Processes
2.4Glacial Landforms
3Option 2B: Coastal Landscapes & Change
3.1Coastal Landscapes
3.2Coastal Erosion & Deposition
3.3Coastal Risks
4Globalisation
4.1Globalisation
4.2Negatives of Globalisation
4.3Global Shift
4.5Culture
4.6Measuring Development
5Option 4A: Regenerating Places
5.1Types of Economies
5.2Function of Places
5.3Regeneration
5.4Regeneration Case Studies
6Option 4B: Diverse Places
6.1Population Structure
6.2Past & Present Connections
6.3Urban & Rural Spaces
6.4Diversity
6.5Urban & Rural Case Studies
6.6Case Study - Tower Hamlets
6.7Case Study - Sturton-le-Steeple
7The Water Cycle & Water Insecurity (A2 only)
7.1Hydrological Processes Global to Local
7.2Influences on the Water Cycle
7.3Water Insecurity
8The Carbon Cycle & Energy Security (A2 only)
8.1The Carbon Cycle
8.2Energy Consumption
8.3Alternative Energy
8.4Growing Demand for Resources
9Superpowers (A2 only)
9.1Superpowers
9.2Hard & Soft Power
9.2.1Hard & Soft Power
9.2.2Emerging Powers - China Rivalry
9.2.3Emerging Powers - Chinese Sources of Power
9.2.4Emerging Powers - Brazil
9.2.5Emerging Powers - Russia
9.2.6Emerging Powers - India
9.2.7Theories of Development
9.2.8Power Case Studies: Chinese One Belt One Road
9.2.9Power Case Studies: Pakistan Nuclear Arms
9.2.10Power Case Studies: OPEC
9.3IGOs, TNCs & Alliances
10Option 8A: Health & Human Rights (A2 only)
10.1Human Development
10.2Role of Governments & IGOs
10.3Human Rights
10.4Interventions
11Option 8B: Migration & Identity (A2 only)
11.1Globalisation & Migration
11.2Consequences of Migration
11.3Nation States
11.4Responses to Global Migration
Jump to other topics
1Tectonic Processes & Hazards
1.1Tectonic Processes & Hazards
1.2Natural Disasters
1.3Natural Disaster Case Studies
1.4Trends & Patterns
2Option 2A: Glaciated Landscapes & Change
2.1Glaciated Landscapes Over Time
2.2Periglacial Landscapes
2.3Glacial Processes
2.4Glacial Landforms
3Option 2B: Coastal Landscapes & Change
3.1Coastal Landscapes
3.2Coastal Erosion & Deposition
3.3Coastal Risks
4Globalisation
4.1Globalisation
4.2Negatives of Globalisation
4.3Global Shift
4.5Culture
4.6Measuring Development
5Option 4A: Regenerating Places
5.1Types of Economies
5.2Function of Places
5.3Regeneration
5.4Regeneration Case Studies
6Option 4B: Diverse Places
6.1Population Structure
6.2Past & Present Connections
6.3Urban & Rural Spaces
6.4Diversity
6.5Urban & Rural Case Studies
6.6Case Study - Tower Hamlets
6.7Case Study - Sturton-le-Steeple
7The Water Cycle & Water Insecurity (A2 only)
7.1Hydrological Processes Global to Local
7.2Influences on the Water Cycle
7.3Water Insecurity
8The Carbon Cycle & Energy Security (A2 only)
8.1The Carbon Cycle
8.2Energy Consumption
8.3Alternative Energy
8.4Growing Demand for Resources
9Superpowers (A2 only)
9.1Superpowers
9.2Hard & Soft Power
9.2.1Hard & Soft Power
9.2.2Emerging Powers - China Rivalry
9.2.3Emerging Powers - Chinese Sources of Power
9.2.4Emerging Powers - Brazil
9.2.5Emerging Powers - Russia
9.2.6Emerging Powers - India
9.2.7Theories of Development
9.2.8Power Case Studies: Chinese One Belt One Road
9.2.9Power Case Studies: Pakistan Nuclear Arms
9.2.10Power Case Studies: OPEC
9.3IGOs, TNCs & Alliances
10Option 8A: Health & Human Rights (A2 only)
10.1Human Development
10.2Role of Governments & IGOs
10.3Human Rights
10.4Interventions
11Option 8B: Migration & Identity (A2 only)
11.1Globalisation & Migration
11.2Consequences of Migration
11.3Nation States
11.4Responses to Global Migration
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