Desertification — AQA A-Level Geography
Test yourself on Desertification with AQA A-Level practice questions.
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Desertification explained
Over the Holocene (the last 10,000 years), hot deserts have fluctuated in extent, notably the Sahara's transition from a green, vegetated state to its current arid distribution due to orbital variations.
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Today, desertification threatens semi-arid margins like the Sahel. This degradation is driven by both natural climate change (prolonged droughts) and human impacts (overgrazing, deforestation, and rapid population growth). The impacts are severe: ecosystems lose biodiversity, landscapes suffer soil erosion, and populations face food insecurity and forced migration. Predicted future climate change threatens to exacerbate these issues, expanding at-risk areas. However, alternative futures exist for local populations through sustainable land management, such as the Great Green Wall initiative, which aims to restore degraded landscapes and secure livelihoods.
Your focus
- Outline the changes in the extent of hot deserts over the past 10,000 years using paleoclimatic evidence.
- Explain the interconnected natural and human causes of desertification in vulnerable regions.
- Evaluate the potential impacts of predicted climate change on the future livelihoods of populations in semi-arid environments.
Desertification exam tips
Marking Points
- Describe the historical fluctuation of hot deserts over the last 10,000 years, referencing evidence of past pluvial periods.
- Analyse the synergistic causes of desertification, balancing natural climate variability with anthropogenic pressures like overcultivation.
- Identify the global distribution of areas at risk of desertification, focusing on semi-arid transition zones such as the Sahel.
- Evaluate the cascading impacts of desertification on ecosystems, landscapes, and human populations.
- Assess predicted climate change scenarios and propose alternative, sustainable futures for affected local populations.
Examiner Tips
- 💡Use the Sahel region as a primary case study to illustrate the complex interplay between human population pressure and fragile ecosystems.
- 💡When discussing the last 10,000 years, refer to the Holocene Climatic Optimum to explain why areas like the Sahara were once much wetter.
- 💡Ensure you explicitly link predicted climate change models to specific socio-economic impacts on local populations, such as reduced crop yields and climate refugees.
Common Mistakes
- Equating desertification with the physical expansion of sand dunes; correction: desertification is the degradation of land in arid, semi-arid, and dry sub-humid areas, primarily involving soil degradation and vegetation loss.
- Blaming desertification solely on human activity; correction: desertification is a complex process driven by the interaction of human impacts and natural climate change.
- Assuming local populations have no agency in future outcomes; correction: alternative futures are possible through mitigation and adaptation strategies, such as agroforestry and water conservation techniques.