Higher Geography SQA
Full course content, a smart revision plan and instant past paper feedback for Higher Geography SQA.
Content Overview
60 topics in 10 modules
☑️ Atmosphere 5 topics
- The Global Heat Budget
- Global Variations in Heat Energy
- Atmospheric Circulation
- Oceanic Circulation
- Intertropical Convergence Zone
☑️ Hydrosphere 3 topics
- Hydrological Cycle
- Hydrographs
- The difference between describing and explaining a hydrograph
☑️ Lithosphere 9 topics
- Glaciation
- Erosional Features
- Depositional Features
- Fluvio-glacial features
- Glaciated uplands on an OS map
- Rural land use conflicts: The Lake District
- Coasts
- Coasts on OS maps
- Rural land use conflicts: Dorse Coast
☑️ Biosphere 7 topics
- Soils
- Soil formation
- Factors determining soil type
- Soil profiles and processes
- Brown earth
- Podzol
- Gley
☑️ Population 9 topics
- The growing world population
- Census
- Case Study: Nigeria
- Other ways to collect demographic data
- Population data presentation
- Consequences of population structure
- Migration
- Causes and impact of vonutary migration
- Causes and impact of forced migration
☑️ Rural 6 topics
- Rural land degradation in north Africa
- Physcical causes of desertification
- Human casues of desertification
- Consequences of desertification
- Possible solutions to desertification
- Case Study: Tigray, Ethipoia
☑️ Urban 5 topics
- The urban population
- Urban change and management in a developed world city: Glasgow
- Changes to Housing
- Changes to Transport in Glasgow
- Urban change and management in a developed world city: Kibera, Nairobi, Kenya
☑️ River Basin Management 6 topics
- Case Study: The Colorado basin, USA
- Factors when consideriing the site of a dam
- Global water surplus and deficiency
- Hoe can river basins be managed?
- Multi-purposeriver basin management
- Why the world needs water management
☑️ Development and Health 6 topics
- Indicators of development
- Relationship between social and economic indicators
- Inequalities between developing countries
- Malaria-water related diseases
- Improving health care in developing countries: Primary Health Care
- Example of WHO's work: Primary Health Care (PHC)
☑️ Global Climate Change 4 topics
- Causes of Climate Change
- Local Impacts of climate change
- Global impact of climate change
- Management strategies and their limitations
Higher Geography SQA Revision Content
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Higher Geography SQA - Atmosphere - The Global Heat Budget Content Preview
Atmosphere
The Global Heat Budget
The Global Heat Budget
basic understanding
- The Global Heat Budget refers to the balance of incoming and outgoing solar radiation that warms the Earth and atmosphere.
- Essentially, it is an expression of how the planet attempts to maintain a delicate energy equilibrium.
- Understanding this, is key to comprehend more complex atmospheric phenomena such as weather patterns, greenhouse effect and climate change.
insolation and albedo
- The Sun's energy, called insolation, reaches Earth's atmosphere and approximately 30% of it is reflected back into space. This is due to albedo, or the reflective properties of different surfaces.
- For example, surfaces such as snow and ice are highly reflective with high albedo rating, while asphalt road or dark forests have lower albedo.
- The remaining 70% of insolation is absorbed by the Earth's surface and atmosphere, warming the planet.
heat transfers: conduction, convection and radiation
- The absorbed solar energy is redistributed around the planet through three methods of heat transfer: conduction, convection, and radiation.
- Conduction is the process of heat transfer from a hot object to a colder one when they come in contact with each other.
- Convection pertains to heat transfer where warm air rises and cool air sinks, making a continuous circulation.
- Radiation is the emission of energy as electromagnetic waves where no physical medium is needed for it to travel.
terrestrial radiation and the greenhouse effect
- As Earth's surface absorbs solar radiation, it also emits radiation back into the atmosphere; this is called terrestrial radiation.
- Some of this re-emitted radiation escapes back into space, but a lot is absorbed by certain gases in atmosphere, known as greenhouse gases, that re-radiate the energy back towards the Earth. This is known as the Greenhouse Effect.
- Some of these greenhouse gases include carbon dioxide (CO2), methane (CH4), and water vapor (H2O).
- This trapping of heat is crucial to supporting life on the planet as it keeps the Earth's average temperature at a habitable level. However, an increase in the concentration of these gases can lead to global warming and climate change.
To summarise, the Global Heat Budget describes the delicate balance of insolation, reflection, absorption, and re-radiation that maintains the Earth's climate. Understanding these points will clarify on how disturbances can lead to significant climatic changes. Be sure to understand the roles of albedo, modes of heat transfer, and the greenhouse effect in this balance.
Question: What are the three methods of heat transfer involved in the global heat budget, and how does each process contribute to the redistribution of the Earth's heat?
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