C2.10

Global warming

Indicative relationship: Activate 1 · Chemistry contextual consolidation
KS3 science lesson

Global warming

Lesson focus: How can gases change Earth’s ?

Learning objective

Explain the greenhouse effect and connect it to changes in atmospheric composition.

Build on earlier learning

Carbon cycle

Connect atmospheric carbon changes to their effects on energy transfer.

You will be successful when you can…

  • Distinguish sunlight and infrared radiation.
  • Describe greenhouse-gas absorption and emission.
  • Explain temporary energy imbalance.
  • Connect fossil carbon to warming.
KEY VOCABULARY

Words that carry the science

infrared radiation
Electromagnetic radiation emitted strongly by Earth because of its temperature.
greenhouse gas
Atmospheric gas that absorbs and emits infrared radiation at particular wavelengths.
energy balance
State in which incoming and outgoing energy rates are equal.
emission
Release of electromagnetic radiation.
absorption
Transfer of radiation energy into matter.
BUILD YOUR UNDERSTANDING

Explain warming through infrared energy transfer and restored balance

01Sunlight enters, infrared leaves

Earth absorbs mainly shortwave solar energy and emits . Some outgoing infrared escapes directly to space. In simple steps: sunlight warms the Earth’s surface. The warm surface gives off (heat radiation).

02Greenhouse gases absorb and emit

Water vapour, carbon dioxide, methane and other gases absorb particular infrared wavelengths and emit infrared in all directions, including upward and downward. is a : it absorbs some of this infrared and sends some back down to the surface. With more carbon dioxide, less heat escapes to space, so energy builds up and the Earth gets warmer.

03A changed atmosphere changes balance

More greenhouse gas can initially reduce outgoing energy for the same surface temperature. Energy accumulates and the surface/troposphere warm until outgoing energy again matches incoming energy.

Shortwave sunlight passes through the atmosphere to Earth. Earth emits infrared radiation upward; some escapes to space and some is absorbed and emitted by greenhouse gases both upward and downward.sunlightinfraredsome escapesto spacesurface absorbs energy and emits infraredatmosphere emits infrared both upward and downward
Figure · Greenhouse gases do not block all heat. They absorb and emit some outgoing infrared radiation. Increasing their concentration changes energy transfer, causing warming until incoming and outgoing energy balance again.
Interactive model

Carbon dioxide and global temperature

Since 1958, carbon dioxide in the air has been measured at Mauna Loa in Hawaii. Plot it against the average global temperature: as carbon dioxide has risen, so has the temperature. The greenhouse effect explains why.

421.1 ppm+1.17 °CCarbon dioxideTemperature change2023

Controls

2023
Carbon dioxide421.1 ppm (before 1800: about 280 ppm)
Temperature change+1.17 °C vs 1951–1980

Approximate, rounded values (NOAA Mauna Loa carbon dioxide; NASA GISTEMP temperature). A correlation alone does not prove cause; the greenhouse effect gives the mechanism.

The points slope upwards: years with more carbon dioxide in the air have higher global temperatures.320340360380400420-0.4-0.20.00.20.40.60.81.01.21.42023Carbon dioxide / ppmTemperature change / °C
WORKED EXAMPLE

Use a simple energy budget

Incoming absorbed energy is 240 units; outgoing energy falls temporarily from 240 to 238 units.

  1. Initial balance: 240 in and 240 out.
  2. After change: 240 in and 238 out.
  3. Net gain = 2 energy units per time.
  4. Warming raises outgoing infrared until balance is restored at a higher temperature.

How to make the reasoning visible: Persistent warming requires an energy imbalance, not energy appearing from nowhere.

LEARN BY DOING

Radiation pathway check

Label each arrow by radiation type, direction and interaction.

Arrow/eventRadiationDirectionOutcome
Sun to surfaceMostly shortwaveDownAbsorbed/reflected
Surface emissionInfraredUpEnergy leaves surface
Atmospheric absorptionInfraredInto gasesMolecules gain energy
Atmospheric emissionInfraredUp + downSome escapes/some returns
Space escapeInfraredUpEarth-system energy loss
  1. Why is “greenhouse gases block all heat” wrong?

  2. How does warming help restore balance?

  3. Use the table. What happens to some of the infrared radiation that greenhouse gases absorb?

RETRIEVE · APPLY · CHECK

Check your understanding

Answer from memory, then check against the suggested answer.

What is infrared radiation?

What is greenhouse gas?

What is energy balance?

Name one greenhouse gas.

What type of radiation does the Earth give out?

Apply the idea

Connect fossil-fuel combustion to warming.

Stretch and challenge

Why does downward infrared not violate conservation of energy?

Why does burning more fossil fuels add to global warming?

Exam Question Practice

C2.10Explain5 marks

Exam Question Practice

Mark points shown after marking

Answer the parts to explain how more carbon dioxide in the air can make the Earth warmer.

(a)

Sunlight warms the Earth’s surface. What does the warm surface give off?

(1)
(b)

What does carbon dioxide do to some of that infrared?

(1)
(c)

With more carbon dioxide, what happens to the heat escaping to space?

(1)
(d)

So what builds up?

(1)
(e)

So what happens to the temperature?

(1)

Total for this question: 5 marks

Command word: Follow the heat step by step. Carbon dioxide does not block all heat.

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