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NotesESSTopic 6.4The ozone layer
Back to ESS Topics
6.4.36 min read

The ozone layer

IB Environmental Systems and Societies • Unit 6

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Contents

  • Where the ozone is
  • Ozone absorbs UV and protects life
  • Good ozone up high, bad ozone nearby
  • Reading an ozone profile
  • Exam-style question
A thin shield, high up: Ozone is spread through the air, but most of it sits in the stratosphere. The part with the most ozone is called the ozone layer.

The points to remember

  • Ozone (O₃) is a gas made of three oxygen atoms.
  • About 90% of all ozone is in the stratosphere; about 10% is in the troposphere.
  • The ozone layer is the part of the stratosphere with the most ozone: about 15 to 35 km up.
  • The peak is usually at about 20 to 25 km; it is higher over the tropics and lower near the poles.
  • There is very little of it: brought down to the ground, all the ozone would make a layer only about 3 mm thick.
Ozone concentration against altitude over the tropics: very low near the ground and in the troposphere, rising above about 16 km to a peak at about 26 km, then falling to almost nothing by 40 km; the band of highest concentration is labelled 'Ozone layer'
Most ozone sits in one layer high in the stratosphere.

Real example: in the 1920s the British scientist Gordon Dobson built an instrument that measures how much ozone is in the air above it by reading sunlight. The amount is still given in Dobson units, and typical values are 200 to 500.

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The job of the ozone layer is to absorb UV. Every bit of UV it absorbs is UV that never reaches living things on the ground.

The points to remember

  • Stratospheric ozone absorbs UV radiation from the Sun.
  • It absorbs all UVC and most UVB, so much less UV reaches Earth's surface.
  • UV is harmful because it is high-energy radiation, especially the shortest wavelengths.
  • So the ozone layer protects living organisms from UV damage: DNA, skin, eyes, plants and plankton.
  • Absorbing UV also warms the stratosphere: it gets warmer with height.

Sun's UV

  • UVA, UVB and UVC arrive at the top of the atmosphere.

Ozone layer

  • Absorbs all UVC and most UVB, 15-35 km up.

Surface

  • Much less UV reaches plants, animals, plankton and people.
Remember it as: Ozone absorbs, so less UV arrives, so life is protected.

Real example: Mars has almost no ozone layer. UV at its surface is strong enough to kill unprotected bacteria within minutes, which is one reason scientists look for signs of life under Mars's surface, not on it.

Say what it absorbs AND why it matters: 'It protects life on Earth' or 'it absorbs the Sun's rays' is too vague. Write: 'ozone absorbs UV, so less UV reaches the surface, so less damage to DNA'.

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Ozone is the same gas everywhere, but where it is changes what it does: good up high, bad nearby.

The points to remember

  • Up high (stratosphere): good ozone; it absorbs UV and protects life.
  • Near the ground (troposphere): bad ozone; a pollutant in summer smog.
  • Ground-level ozone irritates lungs and eyes and damages plants and materials.
  • Ground-level ozone does not cause skin cancer or cataracts: those come from UV.
  • The ozone layer is not the greenhouse effect: one absorbs incoming UV, the other outgoing infrared.
Ozone concentration against altitude above a large polluted city: a bulge of ozone near the ground, low values in the rest of the troposphere, and the ozone layer peaking at about 22 km
Above a polluted city: bad ozone near the ground, good ozone high up.

Stratospheric ozone (good)

  • About 15-35 km up
  • Forms the ozone layer
  • Absorbs UVC and most UVB
  • Protects life: we want more

Ground-level ozone (bad)

  • At ground level
  • Part of summer smog
  • Irritates lungs and eyes; damages crops
  • A pollutant: we want less

Real example: on hot, sunny days Los Angeles issues smog alerts: sunlight turns car exhaust into ground-level ozone, and people with asthma are told to stay indoors.

Papers give a graph of ozone against altitude, then ask where the peak is and what the ozone there does for living things. Practise on this one.

Ozone concentration against altitude over the middle latitudes: the peak is at about 22 km, inside the band labelled 'Ozone layer'; the dashed line at 12 km separates troposphere and stratosphere
Over the middle latitudes the peak is at about 22 km.

The points to remember

  • Identify the altitude: find the widest point of the curve, read across, and give the unit (km).
  • Point 1: ozone absorbs UV from the Sun, so less ozone = more UV at the surface.
  • Point 2: UV harms living tissue: cataracts, mutations in dividing cells, skin cancer, a weaker immune system.
  • Point 3: UV damages leaves, algae and phytoplankton, so less photosynthesis.
  • Point 4: so less food up the food chain, e.g. fewer krill around Antarctica.
  • Never just 'it protects life' or 'it absorbs the Sun's rays'; never 'global warming'.
1

Read the peak

About 22 km: write the unit, or the mark is lost.

2

Absorbs UV

Less ozone at 20-30 km lets more UV reach the ground.

3

Harm

Cataracts, mutations, skin cancer; damaged phytoplankton.

4

Food chain

Less photosynthesis, so fewer krill in the Southern Ocean.

Three answers that score nothing: '22' with no unit. 'It protects life on Earth'. 'Less ozone causes global warming': ozone loss is not a cause of climate change.

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How this comes up: Paper 2, Section A (May 2025, all three time zones): (a) read the altitude of the peak [1], then (b) what the ozone there does for living things [2].
Ozone concentration against altitude above a city, peak at about 22 km
Ozone above a city.
IB-style questionDescribe[3 marks]

The figure shows the concentration of ozone at different altitudes above a large city.

(a) Identify the altitude with the highest concentration of ozone.

(b) Describe how a decreased concentration of ozone between 20 and 30 km could affect living organisms.

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A science museum display says that the ozone layer 'protects us from the Sun'.

the term ozone layer.
[2 marks]

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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6.4.2Ultraviolet radiation
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