This topic explores the natural causes of climate change throughout Earth's history, focusing on the Quaternary period, and examines the evidence used to r
Topic Synopsis
This topic explores the natural causes of climate change throughout Earth's history, focusing on the Quaternary period, and examines the evidence used to reconstruct past climates.
Key Concepts & Core Principles
- Milankovitch cycles: Long-term changes in Earth's orbit (eccentricity, obliquity, precession) that alter the amount and distribution of solar radiation, driving glacial-interglacial cycles.
- Volcanic eruptions: Major eruptions (e.g., Mount Pinatubo, 1991) can inject aerosols into the stratosphere, reflecting sunlight and causing temporary global cooling.
- Solar output variations: Changes in the Sun's energy output (e.g., sunspot cycles) can influence Earth's climate, though the effect is small compared to other factors.
- Evidence for past climate: Ice cores (trapped air bubbles show CO2 and temperature), tree rings (width indicates growth conditions), and ocean sediments (foraminifera shells record sea surface temperatures).
- Feedback mechanisms: Positive feedbacks (e.g., ice-albedo feedback: melting ice reduces reflectivity, causing more warming) amplify natural climate changes.
Exam Tips & Revision Strategies
- Ensure you can distinguish between natural causes of climate change and human-induced (enhanced greenhouse effect) causes
- Be prepared to explain how specific pieces of evidence, such as ice cores or tree rings, provide data on past climates
Examiner Marking Points
- Understanding of glacial and interglacial periods during the Quaternary period
- Identification of natural causes of climate change: Milankovitch cycles, solar variation, and volcanism
- Identification of evidence for natural climate change: ice cores, pollen records, tree rings, and historical sources