aımnova
DashboardMy LearningCrash CoursesStudy Plan

Aimnova site navigation

Stay in the loop

Get the latest study resources and updates

New features, study tips and exam insights — straight to your inbox.

IB Diploma

  • IB Past Papers
  • IB Study Notes
  • IB Question Bank
  • IB Mock Exams
  • IB Revision

IB Subjects

  • IB Math AA
  • IB Math AI
  • IB Economics
  • IB Business Management
  • IB Physics
  • IB Biology
  • View all IB subjects→

IB Past Papers

  • IB Math AA HL Past Papers
  • IB Math AA SL Past Papers
  • IB Math AI HL Past Papers
  • IB Math AI SL Past Papers
  • IB Economics HL Past Papers
  • IB Economics SL Past Papers
  • IB ESS Past Papers
  • View all past papers→

Study Resources

  • Study Notes
  • Question Bank
  • Mock Exams
  • Crash Courses
  • Flashcards
  • Revision Guide
  • Exam Skills
  • Command Terms
  • Grade Calculator
  • Exam Timetable 2026

Aimnova

  • Features
  • Pricing
  • For Teachers
  • For Schools
  • For Parents
  • About Us
  • Blog
  • Contact
aımnova

IB study, practice and feedback built around the real exam.

TermsPrivacyCookies·© 2026 Aimnova. All rights reserved.c1e448f

Aimnova is not affiliated with or endorsed by the International Baccalaureate Organization (IB).

NotesPhysics HLTopic 2.2Greenhouse effect and greenhouse gases
Back to Physics HL Topics
2.2.46 min read

Greenhouse effect and greenhouse gases (Physics HL)

IB Physics · Unit 2

Your first topic is free to keep

Know exactly what to write for full marks

Practice with exam questions and get AI feedback that shows you the perfect answer — what examiners want to see.

Start Free

Contents

  1. 1What the greenhouse effect is
  2. 2How greenhouse gases trap heat
  3. 3Exam-style question
The big idea: Climb into a car left in the Sun and it's like an oven inside — the windows let sunlight in but trap the heat. Some gases in the air do the same to the whole planet.

How the greenhouse effect works

  • Infrared (IR) is the invisible 'heat' radiation a warm surface gives off — longer-wavelength than visible light.
  • These greenhouse gases absorb that infrared and send some of it back down, keeping the surface warmer.
  • That warming is the greenhouse effect.
Greenhouse gasWhere it comes fromWhy it traps heat
Carbon dioxide, CO2Burning fossil fuels (coal, oil, gas), deforestationIts bonds vibrate at infrared frequencies, so it absorbs Earth's infrared
Methane, CH4Farming (cattle), rice fields, landfill, gas leaksStrong infrared absorber per molecule — even small amounts matter
Water vapour, H2OEvaporation from oceans, lakes and plantsThe biggest natural contributor; absorbs over a wide infrared range
Nitrous oxide, N2OFertilisers, some industryAbsorbs infrared the other gases miss; long-lived in the air

Every one of these gases has natural sources as well as human ones. The human part is what strengthens the effect:

GasNatural sourcesHuman sources
CO₂Respiration, decay, volcanoesBurning fossil fuels, deforestation, cement
CH₄Wetlands, termitesCattle, rice fields, landfill, gas leaks
H₂OEvaporation from oceans and lakesLittle directly; a warmer climate holds more water vapour
N₂OBacteria in soils and oceansFertilisers, some industry
Spot it: Sunlight in (visible) → ground warms → Earth radiates infrared out → greenhouse gases catch some and send it back.

Without them Earth would be about 33 °C colder — far too cold for life. The greenhouse effect is natural and necessary; the problem is making it stronger.

Free preview

This is the free notes preview

You're reading the free notes. Aimnova Pro unlocks the full study experience — and you can try it with your first topic free to keep:

  • FlashcardsLock in vocabulary and key terms with spaced repetition.
  • Practice questionsAnswer exam-style questions and get instant AI marking.
  • Mock exams & past-paper vaultSit full mocks and see exactly how examiners award marks.
  • Personalised study planA daily plan built around your exam date and weak areas.
Start Studying Free Full access to Aimnova Pro · cancel anytime

Follow one packet of energy from the Sun to the ground and back. The key step is the middle one — what the gas molecules do to infrared:

StepWhat happens to the energy
1 · Sunlight inShort-wave sunlight (mostly visible) passes through the atmosphere and warms the ground
2 · Earth radiatesThe warm surface re-emits this energy as longer-wavelength infrared radiation
3 · Gases absorbGreenhouse-gas molecules (CO2, CH4, H2O, N2O) absorb that infrared — their bonds resonate at infrared frequencies
4 · Re-emit (some back down)The molecules re-emit infrared in all directions — so some is sent back down to the surface
5 · Trapped → warmerThat returned energy keeps the surface warmer than it would be with no atmosphere
Why these gases — and not nitrogen or oxygen: A molecule absorbs infrared only if its bonds can vibrate at infrared frequencies — this is called resonance (the radiation's frequency matches the bond's natural vibration).

Absorb infrared

  • CO2, CH4, H2O and N2O have bonds that resonate at infrared frequencies.
  • So they absorb Earth's infrared.

Let infrared through

  • The main air gases N2 and O2 do not.
  • Their simple two-atom bonds don't vibrate that way, so they let infrared straight through.
Two ways to explain the absorption: Resonance model: the bonds have natural frequencies in the infrared; radiation at those frequencies drives them and is absorbed.

Energy-level model: a molecule has fixed vibrational energy levels; it absorbs a photon only if hf equals the gap between two levels, then re-emits a photon of the same energy in a random direction.
An infrared photon from the surface is absorbed by a CO2 molecule because its energy matches a gap between energy levels; the molecule re-emits infrared in all directions
The energy-level model: absorb when hf = E₁ − E₀, re-emit in all directions.
The two-way street: When a greenhouse-gas molecule re-emits, it radiates in all directions — not just upward.

So a fraction goes back down to the surface. That returned infrared is the extra warming the greenhouse effect provides.

Get feedback like a real examiner

Submit your answers and get instant feedback — what you did well, what's missing, and exactly what to write to score full marks.

Try AI Tutor FreeYour first topic is free to keep • No credit card required

How this is tested — this micro is mostly words, tested two ways:

Paper 1A

  • A quick 'identify' MCQ — the main human cause of the enhanced effect (burning fossil fuels → more CO2).

Paper 2

  • A short 'outline' of the mechanism: gases absorb the surface's infrared and re-emit some back down.
The classic trap: Saying the gases stop sunlight coming in. They don't — sunlight passes through; the gases trap the infrared Earth radiates back out.
Natural vs enhanced: Natural greenhouse effect = the warming from gases that have always been there.

Enhanced greenhouse effect = the extra warming from gases we add — mainly CO2 from burning fossil fuels. That extra warming is global warming.
Natural greenhouse effectEnhanced greenhouse effect
CauseNaturally present H2O, CO2, CH4, N2OExtra CO2 and CH4 from human activity
Driven byAlways been thereBurning fossil fuels, farming, deforestation
EffectKeeps Earth ~33 °C warmer — needed for lifeExtra warming on top → global warming

The words to know

WordWhat it means
Greenhouse gasA gas that absorbs and re-emits infrared: CO₂, CH₄, H₂O, N₂O
Greenhouse effectWarming of the surface by infrared re-emitted downwards by greenhouse gases
Enhanced greenhouse effectThe extra warming caused by greenhouse gases added by human activity
ResonanceStrong absorption when the radiation frequency equals a natural frequency of the molecule
IB-style questionOutline[2 marks]

Outline the mechanism by which greenhouse gases such as carbon dioxide cause the surface of the Earth to be warmer than it would be with no atmosphere.

Model answer plan

See the answer broken into clear points, with guidance on how each point earns marks.

Claim your free topic
What if there were no atmosphere?: The solar intensity arriving would be the same (it depends only on the Sun and the distance). But with no back-radiation, the surface would be cooler and so would emit less: about 255 K instead of about 288 K.

Try an IB Exam Question — Free AI Feedback

Test yourself on Greenhouse effect and greenhouse gases. Write your answer and get instant AI feedback — just like a real IB examiner.

two greenhouse gases whose atmospheric concentration is increased by human activity, and for each give one human source. [2 marks]

Related Physics HL Topics

Continue learning with these related topics from the same unit:

2.1.1Internal energy and the particle model2.1.2Specific heat capacity2.1.3Latent heat and calorimetry2.1.4Conduction, convection and radiation
View all Physics HL topics
Improve your exam techniqueCommand terms, paper structure, and mark-scheme tips for Physics HL
Previous2.2.3Albedo and Earth's energy balanceNextPressure, volume and temperature relationships2.3.1

22 questions to test your understanding

Reading is just the start. Students who tested themselves scored 82% on average — try IB-style questions with AI feedback.

Start FreeView All Physics HL Topics