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How and why has the climate changed through the Quaternary period and today?

Climate change through the Quaternary period: the evidence for past climate change, the natural causes of climate change, the enhanced greenhouse effect and the human causes of recent warming, and the consequences of contemporary climate change.

An Eduqas GCSE Geography A (C111) answer to climate change through the Quaternary period in Theme 5, covering the evidence for past climate change, the natural causes, the enhanced greenhouse effect and human causes of recent warming, and the consequences of contemporary climate change.

Generated by Claude Opus 4.813 min answer

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  1. What this dot point is asking
  2. Evidence for Quaternary climate change
  3. Natural causes of climate change
  4. The greenhouse effect and human causes
  5. The consequences of contemporary climate change
  6. Try this

What this dot point is asking

This is the opening idea of Eduqas GCSE Geography A (C111) Theme 5, Weather, Climate and Ecosystems, a core theme in Component 2, Environmental and Development Issues. Eduqas expects you to know the evidence for climate change through the Quaternary period (the last 2.6 million years), the natural causes of climate change, the enhanced greenhouse effect and human causes of recent warming, and the consequences of contemporary climate change.

Evidence for Quaternary climate change

The Quaternary is the most recent geological period, the last 2.6 million years, marked by repeated ice ages (cold glacials) and warmer interglacials. We know the climate changed from several lines of evidence.

Natural causes of climate change

Climate changed long before humans, through natural processes.

  • Orbital (Milankovitch) cycles: slow changes in the shape of the Earth's orbit, the tilt of its axis and its wobble alter how much solar energy reaches the Earth, over tens of thousands of years, driving the glacial-interglacial cycle.
  • Solar output: the Sun's energy varies with sunspot activity; fewer sunspots mean a slightly cooler Earth.
  • Volcanic eruptions: large eruptions throw ash and sulphur high into the atmosphere, reflecting sunlight and cooling the planet for a year or two.

The greenhouse effect and human causes

The greenhouse effect is natural and necessary: greenhouse gases (carbon dioxide, methane, water vapour) trap some of the Sun's heat, keeping the Earth warm enough for life. The problem is the enhanced greenhouse effect.

  • Humans release extra greenhouse gases by burning fossil fuels (power, transport, industry), deforestation (fewer trees to absorb carbon dioxide), farming (methane from livestock and rice paddies) and industry.
  • These gases trap more heat, so the planet warms rapidly, far faster than the natural cycles, which is why recent warming is described as human-caused (anthropogenic).

The consequences of contemporary climate change

Warming has wide consequences.

  • Melting ice and rising sea levels: glaciers and ice sheets melt, and warmer water expands, raising sea levels and threatening low-lying coasts and islands.
  • More extreme weather: more frequent and intense heatwaves, droughts, storms and floods.
  • Shifting ecosystems: species move towards the poles or higher ground, growing seasons change, and some habitats and species are lost.
  • Human impacts: threats to water supplies, farming, health and homes, with the poorest and lowest-lying countries most at risk.

Try this

Q1. Explain how ice cores provide evidence of past climate. [4 marks]

  • Cue. Layers of ancient ice trap air bubbles whose carbon dioxide and oxygen isotopes reveal past temperatures and gas levels over hundreds of thousands of years.

Q2. Explain one human activity that contributes to the enhanced greenhouse effect. [4 marks]

  • Cue. Burning fossil fuels for power and transport releases carbon dioxide, which traps extra heat and warms the planet.

Exam-style practice questions

Practice questions written in the style of WJEC Eduqas exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.

Eduqas 2019 (style)4 marksDescribe two pieces of evidence for climate change during the Quaternary period. (Component 2)
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A 4-mark "Describe" question assessing AO1, requiring two pieces of evidence. Markers reward two distinct sources described.

Award credit for any two of: ice cores from Antarctica and Greenland trap air bubbles whose carbon dioxide and oxygen isotopes show past temperatures and gas levels over hundreds of thousands of years; tree rings (dendrochronology) are wider in warm, wet years and narrower in cold, dry ones; pollen analysis from peat bogs shows which plants grew, and so the climate, at different times; and historical records (paintings, diaries, harvest dates) document recent centuries. A strong answer describes two sources and what each reveals, not just names them.

Eduqas 2021 (style)6 marksExplain the difference between the natural and human causes of climate change. (Component 2)
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A 6-mark levels-of-response question assessing AO1 and AO2. Markers reward both natural and human causes explained, not listed.

Strong answers explain the natural causes: changes in the Earth's orbit and tilt (Milankovitch cycles) alter how much solar energy reaches the Earth over tens of thousands of years; variations in the Sun's output (sunspots); and major volcanic eruptions throw ash and gas into the atmosphere, blocking sunlight and cooling the planet for a year or two. Then the human causes: burning fossil fuels, deforestation, farming (methane from livestock and rice) and industry release greenhouse gases, especially carbon dioxide and methane, which trap more heat in the enhanced greenhouse effect, warming the planet rapidly. A good answer contrasts the slow natural cycles with the fast recent human-driven warming. Markers reward both causes and the contrast.

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