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NotesESSTopic 6.4
Unit 6 · Atmosphere and Climate Change · Topic 6.4

IB ESS — Stratospheric ozone

Topic 6.4 examines the ozone layer, the causes and consequences of ozone depletion, and the success of the Montreal Protocol. Students study CFCs, UV radiation, and how international cooperation addressed the ozone crisis — often compared with climate change governance in IB ESS exams.

6.4 FlashcardsExam technique guidePractice questions

Key concepts in Stratospheric ozone

Key Idea: Most marks in topic 6.4 come from the Montreal Protocol and the recovery of the ozone layer. Then learn what destroys ozone and why UV matters.

1. The Montreal Protocol (most marks)

  • Signed in 1987; every UN member has ratified it.
  • It phased out CFCs and other ozone-depleting substances (ODSs), with later dates for poorer countries.
  • It worked: few producers, cheap alternatives, a fund to help, and rules tightened as science grew.

2. Depletion and recovery

  • CFCs from fridges, aerosols and foams release chlorine, which destroys ozone.
  • The Antarctic ozone hole grew fast in the 1980s and peaked at 26.6 million km² in 2006.
  • Ozone should return to 1980 levels around 2066 over Antarctica: CFCs last decades.

3. Why ozone matters

  • The ozone layer in the stratosphere absorbs most harmful UV radiation.
  • More UVB causes skin cancer and cataracts, and cuts phytoplankton photosynthesis.
  • The ozone planetary boundary (about 276 DU) has not been crossed, thanks to the Protocol.

How it is examined:

QuestionHow to score
[1] to [2] Describe ozone-hole dataDirection, peak year and values, with units.
[1] Name the cause of the declineCFCs, or chlorine from ODSs.
[2] Outline the effects of ozone depletionMore UVB: skin cancer, cataracts, less phytoplankton growth.
[4] Explain how the data show the Protocol workedCompare before and after 1987, and note the time lag.
[7] to [9] Evaluate or discuss the Montreal ProtocolWhy it worked, its limits, a comparison with climate deals.

Key terms, one line each:

TermIn one line
Ozone-depleting substance (ODS)a chemical, such as a CFC, that destroys stratospheric ozone
CFCa chlorofluorocarbon once used in fridges, aerosols and foams
Ozone holean area where ozone is below 220 Dobson units
Dobson unit (DU)the unit for the amount of ozone in a column of air
UVBultraviolet radiation that damages DNA; ozone absorbs most of it

Last-minute check: answer, then tap to see.

When was the Montreal Protocol signed? 1987.

Which gas in CFCs destroys ozone? Chlorine.

Name two health effects of more UVB. Skin cancer and cataracts.

Why has the ozone layer not recovered yet? CFCs last decades in the air: a time lag.

IB-style questionExplain[4 marks]

The Montreal Protocol is often called the most successful environmental treaty. Explain why the Montreal Protocol worked so well.

Model answer plan

See the mark-by-mark plan — for / against / judgement, with marking guidance — in study mode.

Claim your free topic →

Exam tips

  • For graph data, give the direction, the peak year and values with units.
  • Say chlorine from CFCs destroys ozone; do not blame carbon dioxide.
  • For the Protocol's success, compare the data before and after 1987.
  • Do not confuse the ozone hole with the greenhouse effect.

What you'll learn in Topic 6.4

  • 6.4.1 Radiation from the Sun
  • 6.4.2 Ultraviolet radiation
  • 6.4.3 The ozone layer
  • 6.4.4 Harm from ultraviolet radiation
  • 6.4.5 A natural ozone balance
  • 6.4.6 Ozone-depleting substances
  • 6.4.7 Ozone depletion and its effects
  • 6.4.8 The Montreal Protocol
  • 6.4.9 The ozone planetary boundary

Exam relevance

ESS is assessed through Paper 1 (case study) and Paper 2 (short answer & structured questions). Concepts from this topic may appear in either paper, often combined with data analysis or real-world examples.

Suggested study order: Read the notes for each sub-topic below → test yourself with flashcards → attempt practice questions → review exam technique.

Study resources — 6.4 Stratospheric ozone

6.4.1

Radiation from the Sun

Notes
6.4.2

Ultraviolet radiation

Notes
6.4.3

The ozone layer

NotesFlashcards
6.4.4

Harm from ultraviolet radiation

Notes
6.4.5

A natural ozone balance

Notes
6.4.6

Ozone-depleting substances

NotesFlashcards
6.4.7

Ozone depletion and its effects

Notes
6.4.8

The Montreal Protocol

NotesFlashcards
6.4.9

The ozone planetary boundary

Notes

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Topic 6.4 Stratospheric ozone forms a core part of Unit 6: Atmosphere and Climate Change in IB ESS. Mastering these concepts will strengthen your understanding of connected topics across the syllabus and prepare you for exam questions that require analysis, evaluation, and real-world application.

Frequently asked questions

What does Topic 6.4 Stratospheric ozone cover in IB ESS?
Topic 6.4 covers stratospheric ozone as part of the IB ESS syllabus. Students learn key concepts, definitions, and real-world examples that are tested in Paper 1 and Paper 2 exams.
How should I revise Stratospheric ozone for IB ESS exams?
Start by reading the micro-topic notes to understand each concept, then use flashcards to memorise key terms. Practise exam-style questions to apply your knowledge under timed conditions and review the marking criteria.
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