IB ESS SL 6.4 Stratospheric Ozone Question Bank
Practise IB ESS SL 6.4 by interpreting ozone trends, explaining UV protection and depletion and evaluating Montreal Protocol recovery evidence.
- Syllabus
- First assessment 2026
- Course
- ESS SL
- Level
- SL
Practise IB ESS SL 6.4 by interpreting ozone trends, explaining UV protection and depletion and evaluating Montreal Protocol recovery evidence.

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.
in the troposphere it causes respiratory illnesses / eye/nose/throat irritations / heart failure;
in the stratosphere it prevents entry of UV that is harmful to humans/can cause mutations/skin cancer/tissue damage/cataracts/crop damage; [1 max]
Note: Do not credit responses that simply suggest global warming/climate change as an impact of tropospheric ozone without referring to some direct impact of those phenomena on humans.
Note: Accept "ozone in stratosphere protects humans from UV" WTTE ... (use of "protects humans" implies UV is harmful to humans).
Outline how decreasing stratospheric ozone may impact living organisms.
Decreased stratospheric ozone increases UV radiation that reaches the earth from the sun;
b. UV radiation can harm sensitive species such as marine organisms (e.g. phytoplankton/coral reefs)/amphibians;
c. UV radiation can damage chloroplasts decreasing plant growth/crop yields/photosynthesis;
d. decreased plant growth/sensitive species can have knock on effects on the food chain/web/decrease access to food;
e. UV radiation can cause mutations/skin cancer/cataracts;
f. UV radiation can weaken the immune system;

Figure:Observed and projected changes in global stratospheric ozone
Describe the overall trend in the recorded annually averaged data shown in the stratospheric-ozone chart shown above.
ozone initially declined;
b. ozone stabilized / began to increase slightly;
Note: do not credit descriptions of the projected values
Allow 1 mark for overall decline
Precise dates are not necessary for credit (i.e. accept change occurring around 2000).
State one chemical responsible for the trend in the recorded annually averaged data between 1980 and 1990 shown in the stratospheric-ozone chart shown above.
halons/CFCs/HCFCsHBFCs/ N2O /methyl bromide/methyl chloroform/carbon tetrachloride/ chlorine/bromine:
Note: do not credit HFCs/ODSs
Outline one impact of low concentrations of stratospheric ozone on plants.
a. cell damage on leaves / reduced leaf size/reduced plant growth/ photosynthesis;
b. reduced phytoplankton in oceans;
(d) Identify the year that stratospheric ozone is predicted to return to 1980 levels in the stratospheric-ozone chart shown above. [1]
Identify the year in which stratospheric ozone is predicted to return to 1980 levels in the stratospheric-ozone chart shown above.
Accept any year in range 2041-2043;
Describe two reasons for the projected change in ozone levels after 2020 in the stratospheric-ozone chart shown above.
a. Montreal Protocol resulted in unprecedented international cooperation to address loss of ozone (and its influence still continues);
b. banned use of CFCs/ phasing out of CFCs/ ozone depleting substances /refrigerants/aerosols/recycling of refrigerants;
c. alternatives to CFCs (HFCs/HCFCs) were developed reducing harm to ozone;
d. education/awareness campaigns led to changes in consumer preferences;
e. ozone reforms due to natural reversible chemical reactions/processes / ODSs eventually begin to break down/dissipate;