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4.11.1Theme D — Continuity and change

Causes of Climate Change — IB Biology SL Revision Notes & Topical Questions

5 min read 4 parts Lesson 13 of 14 Unit quiz

📚 IB Biology SL Hub / Topical Revision
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Curriculum Equation Key قوانين الرقم الهيدروجيني والاتزان الأيوني - pH & Acid-Base Equilibrium FormulasFast Exam Solution
pH = -log[H⁺] | pOH = -log[OH⁻] | pH + pOH = 14 | [H⁺][OH⁻] = 10⁻¹⁴
Word Equation & Conditions: الرقم الهيدروجيني = -لوغاريتم تركيز أيون الهيدروجين | pH + pOH = 14
Location & Specifications: الاتزان الأيوني، كيمياء 3 ثانوي، التحصيلي، و AP Chemistry.
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Section 1 of 4The Greenhouse Effect

Short-wave radiation from the Sun warms the surface, which then radiates longer-wavelength heat back towards space.

Natural effect
  • Natural effect Gases such as carbon dioxide and methane absorb heat radiated from Earth's surface and re-emit it, keeping the planet warm enough for life.
Greenhouse gas
  • Greenhouse gas Any gas in the atmosphere that absorbs infrared radiation from the surface and so reduces heat lost to space.
Enhanced effect
  • Enhanced effect Human activities have raised carbon dioxide and methane concentrations, strengthening the effect and causing global warming.
Terminology
  • Terminology The greenhouse effect is natural;
    • global warming is the rise in temperature;
    • climate change is the wider long-term shift in weather patterns.
GasMain human sources
Carbon dioxideBurning fossil fuels, deforestation, peat harvesting, soil degradation
MethaneCattle farming, rice paddies, landfill, fossil fuel extraction

Section 2 of 4Evidence and Correlation

Scientists use patterns in data and an understanding of mechanisms to judge how strongly evidence supports a conclusion.

Evidence and Correlation
Rising concentrations
  • Rising concentrations Carbon dioxide and methane have increased steeply since the industrial revolution, when fossil fuel use began to rise.
Ice cores
  • Ice cores Air trapped in Antarctic ice shows that temperature and carbon dioxide rose and fell together over hundreds of thousands of years.
Positive correlation
  • Positive correlation As one variable increases the other also increases;
    • a negative correlation is when one rises as the other falls.
Correlation versus causation
  • Correlation versus causation A correlation alone does not prove one variable causes the other;
    • mechanisms and other evidence are also needed.

Section 3 of 4Positive Feedback Cycles

Positive feedback amplifies a change and moves a system further from its starting state.

1
Warming melts polar ice and snow, which are light-coloured and reflective, exposing darker land and sea that absorb more heat.
2
Higher temperatures speed up the enzyme-controlled decomposition of organic matter, so decay organisms release more carbon dioxide.
3
Thawing permafrost releases trapped carbon dioxide and methane, the latter produced by methanogenic archaea.
4
Warmer, drier conditions bring more droughts and wildfires, which release carbon dioxide and remove photosynthesising plants.
5
Each effect adds more greenhouse gas or absorbed heat, causing further warming and driving the system towards a tipping point.

Section 4 of 4Exam Checklist & Tips

4.11.1 – Key Points for the Exam

  • Greenhouse gas A gas that absorbs infrared radiation emitted by Earth and so warms the atmosphere.
  • Albedo The fraction of incoming light that a surface reflects.
  • Permafrost Ground that remains frozen throughout the year.
  • Positive feedback A process in which a change causes further change in the same direction.
  • Anthropogenic Caused by human activity.

Common Mistakes

  • Using greenhouse effect and global warming as if they mean the same thing.
  • Saying that correlation proves causation in the carbon dioxide and temperature data.
  • Calling methane a form of carbon dioxide; it is a separate gas, CH₄.
  • Describing positive feedback as a good outcome; it means amplification, not benefit.

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