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

What Is Causing Climate Change

Carbon dioxide has gone up and down for hundreds of thousands of years without any help from us. So how do scientists know this rise is different? The answer is in the evidence — ice cores, tree rings, sediments and thermometers — and in the sheer speed of the change.

📚 What you need to know

What changed, and when

Before the late 1700s, human societies burned wood and used muscle, wind and water for power. The Industrial Revolution replaced that with coal, then oil and gas. Every tonne of fossil fuel burned releases carbon that had been locked underground for millions of years, so it adds to the atmospheric store rather than cycling within it.

Together these explain why the rate of emissions did not just rise but accelerated after about 1950. Around 90% of global carbon dioxide emissions come from industry and burning fossil fuels, with deforestation and agriculture supplying much of the rest.

Deforestation counts twice. Cutting or burning a forest releases the carbon stored in the trees, and it also removes the photosynthesis that was taking carbon dioxide back out. A loss on both sides of the balance.

How we know what the climate used to be like

Thermometer records only go back to the mid-1800s. To go further we use proxies: natural records that preserve a signal of past conditions.

EvidenceHow it worksWhat it tells us
Ice coresSnow falls, compresses into ice and traps bubbles of air. Deeper ice is older, so a drilled core is a timeline you can read downwardsDirect samples of ancient atmospheres, giving carbon dioxide and methane concentrations going back hundreds of thousands of years
Tree ringsTrees add one ring a year, and the width depends on growing conditions. Wider rings suggest warmer, more favourable yearsYear-by-year climate for the lifetime of the tree, and further back using timber and dead wood — the technique is called dendrochronology
SedimentsLake and ocean beds accumulate layers containing pollen, shells and the remains of temperature-sensitive organismsIndirect evidence of past temperatures, rainfall and vegetation over very long timescales
Instrumental recordsThermometers, and later satellites and ocean buoys, measuring directlyPrecise measurements since the mid-1800s, confirming the sharp recent warming
Worth knowing: the air bubbles in an ice core are not a proxy at all — they are a genuine sample of ancient atmosphere. That is why the carbon dioxide record is so trusted, and why “we cannot know what the air used to be like” is not a good argument.

The carbon dioxide record

Put the ice-core data on a graph and the pattern is striking. Carbon dioxide swings up and down with the ice ages, in a cycle of roughly 100,000 years, but it stays inside a band — roughly 180 to 300 ppm. Then, in the last two centuries, it leaves the band entirely.

Carbon dioxide over the last 800,000 years natural cycles are real — and the modern rise is not one of them 150 200 250 300 350 400 carbon dioxide / ppm 800 600 400 200 0 thousands of years before now the old ceiling: about 300 ppm today: over 420 ppm Schematic, drawn from the shape of the ice-core record rather than exact published values.
The natural cycles took tens of thousands of years to move 100 ppm. The modern rise has done more than that in about two hundred.
When you describe this graph, the mark is in the comparison, not the shape. Say the rise is larger and far faster than anything in the natural record, and that it starts when fossil fuel use starts.

Correlation, causation and why the case is strong

Ice-core data show carbon dioxide and temperature rising and falling together. On its own that is a correlation, and correlation does not prove causation. Examiners like this point, so make it — but do not stop there, because the full case rests on more than one line of evidence:

Feedback loops that make it worse

Warming does not act alone. It triggers processes that cause further warming, which is positive feedback: the original change is amplified. Two loops appear again and again in exams.

Two positive feedback loops each one feeds its own output back in as a new input ICE AND ALBEDO PERMAFROST temperatures rise snow and ice melt darker surface absorbs more sunlight temperatures rise frozen ground thaws trapped CO₂ and methane escape Albedo is how much sunlight a surface reflects. Ice is high, dark water is low. Negative feedback would do the opposite — damp the change and pull the system back.
Feedback loops are why scientists talk about tipping points: past a certain stage, the system keeps warming even without further emissions.
The naming trap. With climate, the words work backwards from how they sound. Positive feedback amplifies a change and is usually bad news. Negative feedback counteracts a change and is usually good news, because it returns the system towards equilibrium.

Crossing a planetary boundary

Climate change is one of the nine planetary boundaries — thresholds which, once crossed, risk large and hard-to-reverse environmental change. The evidence suggests this boundary has already been crossed.

The Intergovernmental Panel on Climate Change (IPCC) assesses the published science and reports on it. Its findings are consistent: average global temperature has risen by roughly 1.1 °C over the past century with the fastest warming in recent decades, greenhouse gas concentrations have risen sharply because of fossil fuels, deforestation and agriculture, and the consequences already include more frequent heatwaves, storms and floods alongside long-term sea-level rise.

Worked examples

WORKED EXAMPLE

Using the ice-core record, explain how scientists can tell the recent rise in carbon dioxide is not part of a natural cycle. [4]

Step 1: describe the natural pattern Over 800,000 years the concentration cycled between roughly 180 and 300 ppm, following the ice ages. Step 2: compare the level Today it is above 420 ppm — well beyond the top of that natural band. Step 3: compare the rate Natural changes of about 100 ppm took tens of thousands of years. The recent change has been larger and taken about two hundred. Step 4: link to the cause The rise begins with industrial fossil fuel use and accelerates after 1950, matching the pattern of human emissions. Higher than natural, and far faster
WORKED EXAMPLE

Explain how melting Arctic sea ice acts as a positive feedback loop. [3]

Start the loop Rising temperatures melt snow and sea ice, exposing darker ocean and land beneath. The physical change Ice has a high albedo and reflects most incoming sunlight; dark water has a low albedo and absorbs it instead. Close the loop More absorbed energy means more warming, which melts more ice, which lowers albedo further. The change amplifies itself. Melting → lower albedo → more absorption → more melting

💡 Exam tip

⚠ Common mix-up

Up next: Climate Change and Ecosystems — coral bleaching, desertification, sea-level rise and the way whole biomes are being pushed towards the poles.

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