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NotesESSTopic 6.4The ozone planetary boundary
Back to ESS Topics
6.4.96 min read

The ozone planetary boundary

IB Environmental Systems and Societies • Unit 6

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Contents

  • The ozone planetary boundary
  • Reading the ozone hole over time
  • Evidence that the Protocol worked
  • Recovery, and the world avoided
  • Exam-style question
A boundary that held: planetary boundaries are limits that keep the Earth in a safe state. For ozone, the limit is a small loss of the ozone layer. Thanks to the Montreal Protocol, the world has stayed inside it.

The points to remember

  • Planetary boundaries mark a safe operating space for humanity; ozone depletion is one of nine.
  • The ozone boundary is less than 5% below the pre-industrial level of 290 DU: about 276 DU.
  • The global average was 284.6 DU in 2023: the boundary has not been crossed.
  • The Antarctic hole dips far lower each spring, but that is regional and seasonal; the global average is safe.
  • The reason: actions under the Montreal Protocol cut ODSs before ozone fell further.
Bar chart of global average ozone in Dobson units (DU): pre-industrial level 290 DU, global average in 2023 284.6 DU, planetary boundary 276 DU
Global ozone (284.6 DU) is still above the boundary (276 DU).

Real example: in 2023 a team led by Katherine Richardson checked all nine planetary boundaries. Six had been crossed, including climate change and biodiversity. Ozone was one of only three still in the safe zone, at 284.6 DU against a boundary of 276 DU.

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Papers give a graph of the ozone hole over time and ask you to describe it, or to read off a year. Learn the shape of the real record.

The points to remember

  • Describe the direction, the years and the numbers: 'rose from 0.1 in 1979 to 23.6 million km² in 1994'.
  • 1979 to the late 1980s: a rapid increase in the hole's area.
  • 1990s to about 2006: large and fairly stable, peaking at 26.6 million km² in 2006.
  • Since about 2000: fluctuating, with a slight overall decrease; very small in 2002 and 2019.
  • Do not describe the projected part of a graph when asked about the recorded data.
Line graph of the mean area of the Antarctic ozone hole every three years, 1979 to 2024, with a dashed line at 1987 for the Montreal Protocol: 0.1 million km² in 1979, 14.2 in 1985, 23.6 in 1994, 26.6 in 2006 (the highest), 17.8 in 2012, 25.6 in 2015 and 19.6 in 2024
Rapid growth in the 1980s, a plateau from the 1990s, a slow, uneven decline since about 2000.
Remember it as: Up fast, flat at the top, slowly down.

Real example: the largest mean area was 26.6 million km² in 2006. In 2019 it was only 9.3 million km², the smallest since 1982, because a sudden warming of the stratosphere weakened the polar vortex that year.

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Did the Protocol work? Read the data: The guide asks you to use data on the ozone hole over time as evidence. Compare before and after 1987, and be honest about what the data do not yet show.

The points to remember

  • The Protocol was signed in 1987: compare the data before and after.
  • World ODS use fell by about 99%, from 1.66 million ODP tonnes (1989) to 17 thousand (2021).
  • Chlorine in the stratosphere peaked in 1993 and has fallen since.
  • The hole stopped growing in the late 1990s and has slowly begun to shrink: some success.
  • But it has not returned to 1980 levels: long-lived ODSs (and a black market) cause a time lag.
  • So the data support success, but the final judgement must wait for recovery.
Line graph of world use of ozone-depleting substances in thousand ODP tonnes: 1,303 in 1986, 1,658 in 1989, 857 in 1992, 407 in 1995, 208 in 2001, 62 in 2007, 29 in 2013 and 17 in 2021
World use of ODSs fell by about 99% after the Protocol.

Real example: world use of ODSs, measured in ODP tonnes, fell from 1,658 thousand in 1989 to 17 thousand in 2021. The ozone hole kept growing until the late 1990s, then levelled off, which fits a cause with a long time lag.

Both sides: Say what supports success (the hole stopped growing) and what limits the judgement (no full recovery yet; a black market; long-lived ODSs).

Scientists use models to project when ozone will recover, and to imagine the world without the Protocol. Both support the conclusion that the boundary was protected.

The points to remember

  • Ozone should return to 1980 levels around 2040 for most of the world, 2045 in the Arctic, 2066 in the Antarctic.
  • Why it recovers: CFCs banned, alternatives used, refrigerants recycled.
  • Education changed what people buy, and international cooperation continues.
  • Ozone re-forms naturally as the old ODSs slowly break down: the balance tips back.
  • Projections are uncertain: models simplify, behaviour and illegal ODSs are hard to predict.
Table of when ozone returns to its 1980 level: most of the world, 60°S to 60°N, about 2040; the Arctic in spring about 2045; the Antarctic in spring about 2066
Recovery is slowest where the depletion was worst.

Real example: NASA scientists modelled a 'world avoided' with no Montreal Protocol (Newman, 2009). By 2065 about two-thirds of the world's ozone would have gone, and the midsummer UV index in cities such as Washington DC would have risen from about 10 to about 30, enough to burn skin in five minutes.

Reasons for the projected recovery: Two reasons, each a full sentence: what was done (the ban, alternatives, recycling, education) and why ozone comes back (ODSs break down, so ozone re-forms).

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How this comes up: Paper 2, Section A, on a graph of the ozone hole or of ozone over time: describe the trend [2], read the year of recovery [1], give two reasons for the projected change [2], or explain how the data judge the Montreal Protocol [4].
IB-style questionExplain[4 marks]

The mean area of the Antarctic ozone hole rose from 0.1 million km² in 1979 to 19.3 million km² in 1987, reached 26.6 million km² in 2006 and was 19.6 million km² in 2024.

Explain how these data can be used to judge the success of the Montreal Protocol.

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IB Exam Questions on The ozone planetary boundary

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How The ozone planetary boundary Appears in IB Exams

Examiners use specific command terms when asking about this topic. Here's what to expect:

Define

Give the precise meaning of key terms related to The ozone planetary boundary.

AO1
Describe

Give a detailed account of processes or features in The ozone planetary boundary.

AO2
Explain

Give reasons WHY — cause and effect within The ozone planetary boundary.

AO3
Evaluate

Weigh strengths AND limitations of approaches in The ozone planetary boundary.

AO3
Discuss

Present arguments FOR and AGAINST with a balanced conclusion.

AO3

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Related ESS Topics

Continue learning with these related topics from the same unit:

6.1.1The atmosphere and its layers
6.1.2Uneven heating and global circulation
6.1.3Greenhouse gases and aerosols
6.1.4The natural greenhouse effect
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