IB ESS SL Topic 6 — Atmosphere & Climate Change Paper 1 & 2 Core idea ~10 min read

How the Greenhouse Effect Works

The greenhouse effect is not pollution, not a problem, and not something we invented. It is a natural process that keeps this planet about 33 °C warmer than it would otherwise be. The trouble only starts when we make it stronger. Getting that distinction right is worth marks in almost every question on this topic.

📚 What you need to know

The gases that do the work

Greenhouse gasWhere it comes fromWhat makes it matter
Water vapourEvaporation from oceans, lakes and rivers; transpiration from plants; sublimation from ice and snow; a product of burning fossil fuelsThe most abundant greenhouse gas. Its concentration depends on temperature, so it amplifies whatever the other gases do rather than driving change itself
Carbon dioxideBurning coal, oil and natural gas; deforestation, which releases carbon stored in trees; industrial processes such as cement productionThe main driver of the enhanced effect, because it is released in huge quantities and stays in the atmosphere for a very long time
MethaneLivestock digestion, landfill, rice paddies, natural gas leaks, wetlandsTraps heat far more effectively than carbon dioxide — over twenty times as much per molecule over a century — but is present in much smaller amounts
Nitrous oxideSynthetic and organic fertilisers, fossil fuel combustion, some industrial processesAround 300 times the warming effect of carbon dioxide per molecule, again at a far lower concentration
Potency versus quantity. Methane and nitrous oxide are individually far stronger, yet carbon dioxide causes more warming overall, because there is so much more of it and it lasts so long. If a question asks why carbon dioxide gets the attention, that is the answer.
Water vapour is usually left out of climate policy, and students find that odd. The reason is that we cannot control it directly: its level is set by temperature. Warm the planet with carbon dioxide and the extra water vapour follows automatically — which is why it is treated as a feedback, not a cause.

Aerosols

Aerosols are tiny solid particles or liquid droplets suspended in the air. Black carbon, produced by incomplete combustion of fossil fuels, wood and other biomass, comes from diesel engines, cooking stoves and open burning. It matters twice over: it absorbs sunlight and warms the air around it, and when it settles on snow and ice it darkens the surface, so less sunlight is reflected and melting speeds up.

The mechanism, step by step

Follow the energy. Every mark in this section comes from getting the order and the wavelengths right.

🧩 The energy path

  1. The Sun emits short-wave radiation, including visible light and ultraviolet.
  2. Most of it passes straight through the atmosphere, because greenhouse gases do not absorb these wavelengths.
  3. Some is reflected by clouds, ice and bright surfaces. The rest is absorbed by the Earth’s surface, which warms up.
  4. The warm surface re-emits that energy at longer wavelengths — infrared, felt as heat.
  5. Greenhouse gases absorb this infrared radiation and re-emit it in all directions, including back down.
  6. Some heat still escapes to space, but less than would without the gases — so the surface stays warmer.
Energy in, energy out — and the bit that stays the wavelength changes at the surface, and that is the whole trick SUN 1 short-wave sunlight passes through 4 some heat escapes to space top of the atmosphere 3 greenhouse gases absorb it and re-emit it in all directions 2 the surface absorbs it and re-emits longer-wave infrared Greenhouse gases are transparent to sunlight but not to infrared. Energy gets in easily and leaves slowly, so the surface settles at a warmer temperature.
Notice that nothing is “trapped” forever. Heat still leaves; it just takes a longer, more roundabout route out.
The blanket comparison is a good one: a blanket does not make heat, it slows the rate at which your heat escapes. Greenhouse gases do the same for the planet.

Natural versus enhanced

Without any greenhouse gases, the infrared leaving the surface would go straight out to space and the average temperature would sit near −18 °C — oceans frozen, and no life as we know it. The natural greenhouse effect lifts that to about 15 °C. Adding more greenhouse gases lifts it further still.

No effect, natural effect, enhanced effect the more greenhouse gas, the smaller the share of heat that gets away NO GREENHOUSE GASES NATURAL EFFECT ENHANCED EFFECT all the heat escapes some heat returns more heat returns about −18 °C about 15 °C warmer, and rising The natural effect is worth about 33 °C. We are adding to it. Only the third panel is a problem — and only because of how fast the change is happening.
The middle panel is what makes Earth habitable. The right-hand panel is what the rest of this topic is about.

The water vapour feedback

Here is the loop that makes carbon dioxide more dangerous than its own absorption suggests. A warmer atmosphere can hold more water vapour. Water vapour is itself a greenhouse gas, so it causes more warming, so the air holds more water vapour again. That is positive feedback: the original change is amplified rather than damped down.

The loop to remember more CO2 → warmer air → more evaporation → more water vapour
→ more warming → back to the start

Worked examples

WORKED EXAMPLE

Explain how the greenhouse effect keeps the Earth’s surface warm. [4]

Step 1: energy arrives The Sun emits short-wave radiation, which passes through the atmosphere largely unabsorbed. Step 2: the wavelength changes The surface absorbs it, warms, and re-emits the energy as longer-wave infrared radiation. Step 3: the gases act Greenhouse gases such as carbon dioxide and water vapour absorb infrared and re-emit it in all directions, including back towards the surface. Step 4: the result Less energy escapes to space than arrives directly at the surface, so the surface settles at a higher temperature — about 15 °C rather than about −18 °C. Short-wave in, long-wave out, some sent back down
WORKED EXAMPLE

Methane traps over twenty times more heat per molecule than carbon dioxide. Explain why carbon dioxide is still considered the more important greenhouse gas. [3]

Accept the fact Per molecule, methane really is far more effective at absorbing infrared radiation. Bring in concentration Carbon dioxide is present at roughly 0.04% of the atmosphere; methane is hundreds of times rarer. Bring in lifetime Carbon dioxide remains in the atmosphere far longer, so emissions accumulate over decades and centuries rather than fading. Potency × quantity × lifetime = total effect

💡 Exam tip

⚠ Common mix-up

Up next: Atmospheric Processes That Drive Climate — how uneven heating, circulation and the water cycle turn that energy balance into the climate of a place.

Want this explained one-to-one?

Book a free session with an experienced IB ESS tutor and get your trickiest topics made simple.

Book a Free Session →