MrBadmusAI
  1. KS3
  2. Chemistry
  3. The Earth and its atmosphere
  4. Carbon dioxide, humans and climate

The Earth and its atmosphere · System

Carbon dioxide, humans and climate

A gas making up four hundredths of one per cent of the air decides the temperature of the planet. Two centuries of burning things has moved that number by half again.

Start here

The Earth absorbs a certain amount of energy from the Sun and radiates the same amount back out to space. Work out the temperature that balance needs and the answer is about −18 °C.

The average surface temperature of the Earth is about 15 °C. Thirty-three degrees have to come from somewhere, and it is not the Sun — the Sun is already in the sum.

Where do the extra thirty-three degrees come from?

Carbon dioxide, methane and water vapour are greenhouse gases. They are transparent to visible light and opaque to the infrared radiation the Earth gives off — and that difference is the entire mechanism.

Since about 1750, human activity has raised the carbon dioxide in the air from around 280 parts per million to over 420 — mostly by burning fossil fuels, with clearing forests and making cement accounting for the rest. That is not a subtle change to a small number. It is an increase of about half.

Watched first · four steps

How the effect actually works

0 of 4 revealed

Most descriptions of this get one step wrong. Reveal them one at a time and watch what the gases do and do not do.

  1. Sunlight passes straight through the atmosphere and warms the ground.

    Coming in · visible light · passes straight through

  2. The warmed ground radiates energy back out — as infrared, not as light.

    Going out · infrared · emitted by the warmed surface

  3. Greenhouse gases absorb infrared and radiate it again in all directions.

    Going out · infrared · absorbed and re-emitted

  4. Energy leaves more slowly than it arrives, so the surface settles at a higher temperature.

    In and out

Key fact

Greenhouse gases let sunlight through and absorb the infrared the warmed surface radiates back out. More of them means energy leaves more slowly, and the surface settles at a higher temperature.

There is more water vapour in the air than any other greenhouse gas, and people sometimes offer that as an argument. It is not one. How much water vapour the air holds is decided by the temperature: warm the air and it holds more, cool it and the extra falls out as rain within days. It follows the temperature rather than setting it. Carbon dioxide does not — it stays in the air for a very long time whatever the weather does, which is why the gas that has changed the climate is the one people added.

Your turn · four pieces of evidence

What does each one actually show?

0 of 4 judged

Decide what each one can and cannot establish on its own.

Evidence 1 · direct measurement

Carbon dioxide has been measured continuously at an observatory in Hawaii since 1958. It has risen every single year, from 315 to over 420 parts per million, with a small saw-tooth wobble each year.

Evidence 2 · ice cores

Bubbles of air trapped in Antarctic ice give a direct sample of the atmosphere going back 800,000 years. Across all of it, carbon dioxide stayed between 180 and 300 parts per million.

Evidence 3 · the chemical fingerprint

Carbon from fossil fuels has a slightly different mix of carbon isotopes — atoms of carbon that weigh slightly different amounts — from carbon released by volcanoes or by the oceans. The extra carbon dioxide in the air carries the fossil fingerprint.

Evidence 4 · the laboratory

Shine infrared through a tube of carbon dioxide and measure what comes out of the other end. The gas absorbs strongly at particular wavelengths. This was first measured in the 1850s.

Key fact

The greenhouse effect is natural and necessary: without it the surface would average about −18 °C instead of about 15 °C. What human activity has changed is its strength, by raising carbon dioxide from about 280 to over 420 parts per million since 1750.

Five words

Say your answer out loud before you turn each card over. If you cannot say it, you do not know it yet.

Think again

“The planet is warming because of the hole in the ozone layer letting extra heat in.”

Both are real problems with the atmosphere. Commit before you read on.

Mastery ladder

Not started yet.

Rungs 3 and 4 you mark yourself.

Rung 1 · Recall

Which of these is the correct description of the greenhouse effect?

Rung 2 · The one that catches people

Is the greenhouse effect a bad thing?

Rung 3 · Explain

Explain how the greenhouse effect keeps the Earth warm, and why increasing carbon dioxide raises the temperature further. Be precise about what the gases do and do not absorb.

Rung 4 · Take it somewhere new

Someone argues that carbon dioxide levels have gone up and down naturally for hundreds of thousands of years, so the current rise is nothing unusual. Using the evidence in this lesson, write a reply that takes the argument seriously.

Key note

Greenhouse gases such as carbon dioxide and methane let sunlight through but absorb the infrared radiation the Earth emits, keeping the surface about 33 °C warmer than it would otherwise be. That effect is natural and the planet would be frozen without it; what has changed is its strength. Burning fossil fuels has raised carbon dioxide from about 280 to over 420 parts per million since 1750, and several independent lines of evidence — direct measurements, ice cores, the chemical fingerprint of the extra carbon, and laboratory work on the gas itself — agree on the cause.

Going further

Ice cores are the best archive on the planet. Snow falling on Antarctica traps air between its flakes; the snow is buried, compressed to ice, and the trapped air becomes a sealed bubble. Drill down and each bubble is a sample of the atmosphere from the year it was buried. Near the top the years can be counted like tree rings; deeper down the ice has been squeezed too thin to count and the dating comes from models of how ice flows. The deepest cores reach back 800,000 years, and across all of that time carbon dioxide moved between roughly 180 and 300 parts per million. It has never, in that entire record, been where it is now.

Some of the consequences are slower than people expect and some are faster. Sea level rises partly because ice on land melts and partly because water expands as it warms — and the ocean is deep, so it takes centuries to warm through. Carbon dioxide already released stays in the atmosphere for a very long time. Methane is a far stronger greenhouse gas per molecule but breaks down within about a decade, which makes it the fastest thing to act on and the reason livestock, landfill and gas leaks get attention out of proportion to their tonnage.

Before this lesson

Connects to

At GCSE this becomes

  • Radiative balance and infrared absorption, evaluating climate models and their uncertainties, and carbon footprints of products and processes.

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