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NotesESS HLTopic 6.2The enhanced greenhouse effect
Back to ESS HL Topics
6.2.47 min read

The enhanced greenhouse effect (ESS HL)

IB Environmental Systems and Societies • Unit 6

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Contents

  • The enhanced greenhouse effect at Higher Level
  • The natural and the enhanced greenhouse effect
  • The greenhouse gases people emit
  • Reading emissions by sector
  • From global warming to climate change
  • Why natural causes cannot explain it
  • Exam-style question
The enhanced greenhouse effect at Higher Level: The same ideas as SL, with different cases: methane's rise, Australia's coal-powered electricity, the Lytton heat and the IPCC's attribution of warming. At HL, practise the long answer: weighing natural against human causes with evidence on both sides.

Practise this as you read

  • Chain every point: gas, heat kept in, warming, climate change.
  • Weigh natural causes with numbers before you dismiss them.

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A natural blanket, made thicker by people: Greenhouse gases keep the Earth warm. Human emissions have added more of them, so they trap more heat.
Diagram: short-wave radiation from the Sun passes through the atmosphere to the surface; the surface gives off long-wave radiation; greenhouse gases re-emit some back down and some heat escapes to space
The natural greenhouse effect keeps the Earth warm enough for life.

The points to remember

  • Short-wave radiation from the Sun passes through the atmosphere and warms the surface.
  • The warm surface gives off long-wave (infrared) radiation.
  • Greenhouse gases absorb this heat and re-emit some of it back down: the natural greenhouse effect.
  • It keeps the Earth at about 15 °C on average instead of about -18 °C: life needs it.
  • Human emissions add more greenhouse gas, so more heat is absorbed and re-emitted: the enhanced greenhouse effect.
The same diagram with a thicker arrow of heat re-emitted back down and less heat escaping to space
The enhanced greenhouse effect: more gas, more heat kept in.
Remember it as: Short-wave in, long-wave out, more gas keeps more in.

Real example: methane in the air is now more than 2.5 times its level in 1750: about 1,936 ppb in 2025, against about 729 ppb before the Industrial Revolution.

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The guide names three gases that people emit in large quantities, and smaller amounts of others. Learn each gas with its human sources.

The points to remember

  • Carbon dioxide: burning fossil fuels, deforestation, cement. Up from about 280 to 427 ppm.
  • Methane: cattle and sheep (digestion), rice paddies, landfill, gas leaks. More than 2.5 times its 1750 level.
  • Nitrous oxide: nitrogen fertilizers, manure, burning fuel. About a quarter higher than in 1750.
  • Smaller quantities of other GHGs: F-gases such as HFCs from fridges and air conditioners.
  • GWP (global warming potential) compares a gas's warming with the same mass of CO2 over 100 years.
  • CO2 has the biggest total effect because there is so much of it: about three-quarters of all emissions.
Table: carbon dioxide 280 ppm before 1750 and 427 ppm in 2025, GWP 1; methane 729 ppb and 1,936 ppb, GWP 27-30; nitrous oxide 270 ppb and 339 ppb, GWP 273; HFCs none and very small, GWP hundreds to thousands
All the main human greenhouse gases have risen since 1750.

Real example: worldwide in 2019, CO2 made up about three-quarters of all greenhouse gas emissions (as CO2-equivalent), methane about 18%, nitrous oxide about 4% and F-gases about 2% (IPCC).

Gas plus source: Link each gas to a human activity: 'methane from the digestion of cattle', not just 'methane'.

Papers give a chart of a country's emissions by sector and ask which sector contributes most.

Grouped bar chart of Australia's emissions by sector in 1990, 2005 and 2021: agriculture 179.4, 141.7 and 128.1; energy 294.7, 425.8 and 427.2; industrial processes 11.6, 11.0 and 17.2; waste 19.5, 15.2 and 13.3 million tonnes
Which sector emits the most?

The points to remember

  • Countries report emissions by sector: energy (including transport), agriculture, industry, waste.
  • Read the key first, then compare bar heights for the year asked.
  • Agriculture is the biggest sector where farming is big and electricity is clean (New Zealand).
  • Energy is the biggest where coal or oil make the electricity (Australia).
  • Emissions are given as CO2-equivalent: each gas converted to the CO2 that would cause the same warming.

Real example: Australia makes much of its electricity from coal, so energy (427.2 million tonnes CO2-eq in 2021) is by far its largest sector; agriculture (128.1) comes second.

Answer the year asked: If the question names a year, compare the bars for that year only, and give the sector's name.

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Warming first, then a changed climate: The enhanced greenhouse effect leads to global warming, and global warming leads to climate change.

The points to remember

  • More GHG means more infrared absorbed and re-emitted, so the global average temperature rises: global warming.
  • A warmer atmosphere changes the whole climate: that is climate change.
  • More evaporation, so heavier rain in some places and drought in others.
  • Winds and precipitation patterns shift; seasons change.
  • More extreme weather: heatwaves, storms, hurricanes, floods.
  • Warming also melts ice and raises sea level.

More CO2

  • Emissions raise the concentration of a greenhouse gas.

More heat kept

  • More infrared absorbed and re-emitted.

Global warming

  • The average temperature rises.

Climate change

  • Evaporation, winds, rain, droughts, storms change.

Real example: on 29 June 2021, the village of Lytton in Canada reached 49.6 °C, Canada's highest temperature ever, during a heatwave that scientists found would have been virtually impossible without human-caused warming.

The climate has always changed naturally. So how do we know the recent warming is human-made? Check each natural cause against what has happened since 1950.

The points to remember

  • Milankovitch cycles: changes in the Earth's orbit and tilt drive ice ages over about 100,000 years: far too slow.
  • Solar output varies by only about 0.1% over an 11-year cycle and has not risen since the 1950s.
  • Volcanic eruptions cause short-term cooling (aerosols reflect sunlight) for a year or two.
  • El Niño and La Niña move heat around for a year or so; they do not add heat over decades.
  • So natural factors cannot explain the fast warming since 1950; the rise in greenhouse gases matches it.

Natural causes

  • Orbit cycles: about 100,000 years
  • Sun: flat since the 1950s
  • Volcanoes: cool for 1-2 years
  • El Niño: a year or so

Human causes

  • Fossil fuels: CO2
  • Deforestation: CO2
  • Farming: methane, nitrous oxide
  • Industry: F-gases, cement CO2

Real example: the IPCC (2021) concluded that it is 'unequivocal' that human influence has warmed the planet: about 1.07 °C of warming by 2010-2019, while natural causes changed the temperature by only -0.1 to +0.1 °C.

Do not say 'the Sun is getting hotter': Solar output has not risen since the 1950s, so it cannot explain the recent warming.

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How this comes up: Paper 2, Section B (c) [9]: weigh natural and human causes of recent warming, with evidence and a conclusion.
IB-style questionTo what extent[9 marks]

Some people argue that the climate has always changed and that today's warming is natural.

To what extent is the global warming observed since 1950 caused by human activity?

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A farmer applies nitrogen fertilizer to increase crop yield.

the greenhouse gas most directly linked to fertilizer use and one reason it contributes to warming.
[2 marks]

Related ESS HL 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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