IB ESS HL 6.4 Stratospheric Ozone Questions

Practise IB ESS HL 6.4 by analysing ozone records and evaluating chemical controls, biological effects and international recovery policy.

Syllabus
First assessment 2026
Course
ESS HL
Level
HL

Exam points

  • Interpret ozone charts by describing long-term decline, stabilisation and projected recovery against 1980 levels.
  • Explain how stratospheric ozone absorbs UV, then link depletion to skin, eye and phytoplankton harm.
  • Identify ODS sources and explain how released halogens catalyse ozone breakdown.
  • Distinguish ozone depletion from global warming by comparing their gases, mechanisms and effects.
  • Evaluate Montreal Protocol success using ozone-hole trends, recovery projections and compliance limits.
  • Evaluate ODS controls and substitutes by weighing ozone benefits against costs and other environmental effects.
  • Explain why HFC replacements require Kigali controls despite reducing ozone harm.

Question 1

[Maximum number: 2]
Tropospheric ozone concentration in Mexico City over time

Figure:Tropospheric ozone concentration in Mexico City over time

Outline why a high concentration of ozone in the troposphere is a direct problem for humans, while in the stratosphere it is a benefit to humans.

Question 2

[Maximum number: 4]

Outline how decreasing stratospheric ozone may impact living organisms.

Question 3

[Maximum number: 7]
Figure 2: Observed and projected changes in global stratospheric ozone

Figure:Observed and projected changes in global stratospheric ozone

Key:
- Annually averaged data
- Average of atmospheric model projections

Question (a)

(a)

Describe the overall trend shown in the recorded annually averaged data in Figure 2.

[ 2 ]

Question (b)

(b)

State one chemical responsible for the trend in the recorded annually averaged data between 1980 and 1990 shown in Figure 2.

[ 1 ]

Question (c)

(c)

Outline one impact of low concentrations of stratospheric ozone on humans.

[ 1 ]

Question (d)

(d)

Identify the year that stratospheric ozone is predicted to return to 1980 levels in Figure 2.

[ 1 ]

Question (e)

(e)

Describe two reasons for the projected change in ozone levels after 2020 in Figure 2.

[ 2 ]

Question 4

[Maximum number: 1]
Figure 2: Observed and projected changes in global stratospheric ozone

Figure:Observed and projected changes in global stratospheric ozone

Key:
- Annually averaged data
- Average of atmospheric model projections

State one chemical responsible for the trend in the recorded annually averaged data between 1980 and 1990 shown in Figure 2.

Question 5

[Maximum number: 3]
Mean ozone-hole area from 1979 to 2016

Figure:Mean ozone-hole area from 1979 to 2016

Question (a)

(a)

State where the ozone hole referred to in the ozone-hole chart shown above is located.

[ 1 ]

Question (b)

(b)

Describe the changes in mean ozone hole area between 1979 and 2016.

[ 2 ]

Question 6

[Maximum number: 1]

Identify one method to reduce ozone-depleting substances.

Question 7

[Maximum number: 9]

The Montreal Protocol on Substances that Deplete the Ozone Layer (1987) is one of the most successful international agreements on a major environmental issue.

Discuss the validity of this statement.

Question 8

[Maximum number: 2]

The hole in the ozone layer over Antarctica, discovered in the 1980s, was caused by chlorofluorocarbons (CFCs). The Montreal Protocol requires the use of hydrochlorofluorocarbons (HCFCs) or hydrofluorocarbons (HFCs) instead of CFCs (Figure 3). However, these two gases are also linked to environmental problems (Figure 4).

Figure 3: Comparison of the effects of CFCs, HCFCs and HFCs

Figure 3:Comparison of the effects of CFCs, HCFCs and HFCs

Figure 4: HCFCs and HFCs cause less damage than CFCs but still affect the environment

Figure 4:HCFCs and HFCs cause less damage than CFCs but still affect the environment

Outline why governments agreed to phase out the use of HFCs from 2019 in the Kigali Amendment to the Montreal Protocol.

All question bank results loaded