Ages

Now you know what causes climate change!

What next?

Try it yourself ↓

What causes climate change?

▶ 5:07 video · Watch on YouTube

  1. 0:00 Snow in a warming world
  2. 0:37 Earth's heat blanket
  3. 1:28 The extra blanket
  4. 2:45 A thicker blanket
  5. 3:36 What a warmer world does
  6. 4:20 Turning it around

Your turn

Run the climate yourself

Play with Earth's blanket!

Each lab is one part of the video. Tap, slide and see what happens.

Each lab isolates one part of the story. The warming and solutions labs are simplified illustrations built on IPCC numbers, not forecasts.

Tap the buttons and slide the sliders.

1

Weather or climate?

Averaging window

Change the averaging window. When does the warming pattern show up?

Monthly values are noisy (illustrative data). Average over 10 or 30 years and the trend emerges from the weather noise.

2

Switch off the blanket

The greenhouse effect

Earth's blanket

Switch the greenhouse gases off, then on. What happens to the thermometer?

Without greenhouse gases the surface would sit near −18 °C; with them, about 15 °C (NASA). A simplified energy-balance picture.

Take the blanket off. Brrr! Now put it back on.

3

Read the Keeling curve

The Mauna Loa record

Drag along the curve (or tap a year). How much carbon dioxide was in the air that year?

Annual Mauna Loa means (NOAA), with an illustrative seasonal wiggle. Drag to read any year from 1958 to 2024.

4

Thicken the blanket

Energy balance

A thicker blanket

Add or remove carbon dioxide. When does more heat come in than goes out?

Toy model: about 3 °C of long-run warming per doubling of CO₂ (IPCC best estimate). Real warming lags because the ocean takes up heat.

Slide it up. What happens to Earth?

5

What is changing?

Observed effects

A warmer world

Tap the numbered spots. What is changing in a warmer world?

Ocean heat, ice loss, sea level, extremes and species shifts: tap each for the observed change (NASA, IPCC).

Tap the numbers. What is changing?

6

Switch to clean

Cutting emissions (a toy)

We can help

Switch each part of the world to cleaner ways. How much warming can we avoid? (A simplified illustration.)

Sector shares from IPCC WG3 (2019) mapped onto the WG1 scenario range (very high ≈ 4.4 °C to very low ≈ 1.4 °C by 2100). Illustrative, not a forecast.

Tap each button. Can you make the sky clear?

What causes climate change?

Weather is the sky today: rain, snow, sun or wind. Climate is what the weather is like over many, many years. A snowy day does not mean Earth is cooling.

Earth's blanket

The Sun warms Earth. Earth gives some of that heat back out. A few gases in the air hold on to part of the heat, like a cozy blanket. We need this blanket, or Earth would be frozen!

A thicker blanket

People burn coal, oil and gas to make power and run cars. Cutting down forests adds more gas too. The extra gas makes the blanket thicker, so Earth gets warmer. It is not the Sun: the Sun is not getting stronger.

What changes?

Ice on mountains is melting, and the sea is rising a little. Hot days are getting hotter, and some animals are moving to cooler places.

Did you know? We know how to fix it! Sun and wind can make clean power, and we can keep forests safe. Every little bit helps. Want to know where the carbon goes? See how the carbon cycle works.

← More explainers

What causes climate change? The short answer

Climate change today is caused mainly by humans adding greenhouse gases to the air, above all carbon dioxide (CO₂) from burning coal, oil and gas.112 These gases act like a blanket around Earth: sunlight gets in easily, but part of the heat Earth gives off is caught and sent back down.2 Add more gas and the blanket gets thicker, so the planet warms.

Before the industrial era, CO₂ was about 280 parts per million (ppm). It is now over 420 ppm, higher than at any time in at least two million years.912 Over the same time, Earth's average temperature has risen by about 1.2 °C since the late 1800s.1012 The world's climate scientists, in the IPCC, call it "unequivocal" that human influence has warmed the atmosphere, ocean and land.12

What is climate change? Weather vs climate

Weather is what the atmosphere is doing over minutes to weeks: a snowstorm, a hot afternoon, a windy week. Climate is the weather averaged over several decades.3 So "climate change" means a long-term shift in those averages, and today it mostly means global warming plus everything warming does to rain, ice, oceans and living things.5

That is why a cold day, or even a cold winter where you live, doesn't disprove warming. One day is weather. The trend over many decades, measured all over the planet, is climate. In the player above, try averaging the same noisy data over one month, then over thirty years: the bumps smooth out and the trend appears.

How the greenhouse effect works

To understand what changes the climate, follow the energy:

  1. Sunlight comes in. About 29% is reflected straight back to space by clouds, tiny particles, ice and snow. The other 71% is absorbed and warms the air, land and ocean.7
  2. Earth glows with heat. A warm planet gives off energy of its own as invisible infrared light.1
  3. Greenhouse gases catch it. Gases such as carbon dioxide, methane, nitrous oxide and water vapour absorb most of that outgoing heat and re-release it in all directions, including back toward the surface.19

This natural greenhouse effect is a good thing. It keeps Earth's average temperature around 15 °C. Without it, the surface would be about 33 °C colder, and much of the planet would be frozen.29 The problem isn't the blanket. It's that we keep making it thicker.

Scientists have known that CO₂ and water vapour trap heat since the 1850s and 1860s, when Eunice Foote and John Tyndall showed it in experiments. In 1896 Svante Arrhenius calculated that more CO₂ would warm the planet.4

The causes of climate change: where the extra gases come from

The IPCC groups global greenhouse gas emissions (2019) by sector:14

SectorShare of emissionsMain sources
Energy supply34%Burning coal, oil and gas for electricity and heat
Industry24%Steel, cement, chemicals
Farming, forests and land use22%Deforestation, livestock, rice, fertilizer
Transport15%Cars, trucks, ships, planes
Buildings6%Heating and cooking with fuels

Fossil fuels are the biggest cause. Coal, oil and gas are the remains of ancient plants and sea life. The carbon in them was pulled out of the air by photosynthesis over millions of years (see how the carbon cycle works), and we are putting it back in a few hundred.9 Other gases add to the blanket too. Methane comes from livestock, rice farming, landfills and leaks from oil and gas systems (natural gas is 70–90% methane). Nitrous oxide comes mostly from fertilizer.1

How does deforestation contribute to climate change?

Trees are made largely of carbon they took from the air. When forests are cleared and burned, or left to rot, that carbon goes back into the atmosphere as CO₂. And fewer trees are left to soak it up again. About half of the emissions from farming and land use are CO₂ from land-use change, mainly deforestation.14 Protecting and restoring forests is one of the ways to slow warming.

The climate change graph: the Keeling curve

In March 1958, scientist Charles David Keeling began measuring CO₂ at the Mauna Loa Observatory, 3,400 metres up a volcano in Hawaii. It is the longest direct record of CO₂ in the air.11 It started at about 315 ppm.9 The line zigzags every year: in the northern spring, growing plants pull CO₂ out of the air, and in autumn, rotting leaves release it.8 But under the zigzag, the curve keeps climbing, and faster over time: about 0.8 ppm per year in the 1960s, and about 2.6 ppm per year in 2015–2024.9 The yearly average at Mauna Loa was 424.6 ppm in 2024.11

Is climate change real? How we know humans are causing it

Yes. Scientists have checked the other suspects:

  • The Sun? Since 1750, the Sun's energy reaching Earth has stayed roughly the same or dropped slightly. And while the lower atmosphere warms, the upper atmosphere is cooling. If the Sun were the cause, both layers would warm. A thicker heat-trapping blanket explains the pattern.1
  • Natural cycles? The IPCC estimates that natural factors (the Sun and volcanoes) changed global temperature by only about −0.1 to +0.1 °C between 1850–1900 and 2010–2019. Human activity accounts for about 1.07 °C.12
  • The CO₂ is ours. CO₂ has risen by nearly 50% since 1750. During the ice-age cycles of the past, it never went above 300 ppm.19

When the blanket thickens, Earth briefly takes in more energy than it gives off. It keeps warming until the two balance again.710 The warming toy in the player uses a simple rule of thumb: about 3 °C of long-run warming for every doubling of CO₂, which is the IPCC's best estimate.12

Effects of climate change: how it affects the environment

A degree or so sounds small, but warming a whole planet takes an enormous amount of energy, and the effects add up:

  • Oceans: the ocean has absorbed about 90% of the extra heat.4 It also absorbs CO₂, which has made seawater about 30% more acidic since the Industrial Revolution (pH 8.21 → 8.10). That makes it harder for corals and shellfish to build their shells.9
  • Ice: glaciers are retreating almost everywhere. Between 1993 and 2019, Greenland lost about 279 billion tonnes of ice per year and Antarctica about 148 billion tonnes.4
  • Sea level: it rose about 20 cm (8 inches) in the last century, from melting land ice and from seawater expanding as it warms. The rate in the last two decades is nearly double that of the last century.4
  • Extreme weather: heat waves are getting more intense and more frequent, and heavy downpours heavier. Every extra half-degree of warming makes these extremes clearly worse.512

How does climate change affect biodiversity and animals?

Plants and animals are on the move. About half of the species scientists have assessed have shifted toward the poles or to higher ground as their homes warm.13 Coral reefs are bleaching, and coral reefs and Arctic ecosystems face a high risk of losing species.13

How does climate change affect humans? Why it matters

Climate change is important because people depend on steady weather, water, crops and coastlines. The IPCC estimates that 3.3 to 3.6 billion people live in places that are highly vulnerable to climate change.13 How much worse it gets depends on our choices. By 2081–2100, the IPCC projects about 1.0–1.8 °C of warming if emissions fall very fast, and 3.3–5.7 °C if they keep rising steeply.12 That gap is why this matters.

Climate change solutions: how to stop climate change

Here's the hopeful part: because we know the cause, we know the fix. To stop the warming, the world must reach at least net zero CO₂, putting no more into the air than is taken out.12 NASA notes that if we stopped adding greenhouse gases, global temperature would level off within a few years.6 And the tools keep getting cheaper. From 2010 to 2019, the cost of solar power fell by about 85%, wind by 55% and lithium-ion batteries by 85%.14

Scientists talk about two kinds of action: mitigation, which means cutting emissions (clean electricity, electric transport, efficient buildings, protecting forests), and adaptation, which means preparing for the changes already happening.6 Every bit of warming we avoid makes a difference.

Common misconceptions

"It's cold today, so there's no global warming." That's weather. Climate is the average over decades, measured across the whole planet.3
"The greenhouse effect is bad." Without it, Earth would be about 33 °C colder. The problem is the extra gases we add.2
"It's just the Sun." The Sun's energy has been flat or slightly lower since 1750, and the upper atmosphere is cooling.1
"One degree is nothing." For a whole planet it is a huge amount of heat, and it's already raising seas and intensifying heat waves.45
"It's too late to do anything." Scientists expect warming to level off within a few years once net CO₂ emissions stop (reach net zero), and every fraction of a degree avoided reduces the harm.612

FAQ

What are the main causes of climate change?

The main cause is burning coal, oil and gas, which adds carbon dioxide to the air. Cutting down forests, farming (which releases methane and nitrous oxide) and some industrial processes add more. These extra greenhouse gases trap more heat, so Earth warms.

How do we know climate change is caused by humans?

Carbon dioxide has risen from about 280 to over 420 parts per million, matching the fossil fuels we burn. The Sun's energy hasn't increased since the 1750s, and natural factors changed global temperature by only about 0.1 °C either way. The IPCC concludes it is unequivocal that human influence has warmed the planet.

What is the difference between weather and climate?

Weather is what the atmosphere is doing over minutes to weeks: rain, snow, sun and wind. Climate is the weather averaged over several decades. One cold day doesn't disprove a warming climate.

Is the greenhouse effect bad?

No, the natural greenhouse effect keeps Earth livable. Without it, the planet would be about 33 °C colder. The problem is the extra greenhouse gas we add, which thickens the blanket and warms Earth further.

How does deforestation contribute to climate change?

Trees store carbon in their wood and roots. When forests are cut down and burned or left to rot, that carbon goes into the air as carbon dioxide, and fewer trees remain to take it back out. Land-use change, mostly deforestation, is a major source of CO2.

How does climate change affect animals and biodiversity?

About half of the species scientists have studied have shifted toward the poles or to higher ground as their homes warm. Warmer oceans are bleaching coral reefs (and more acidic water makes it harder for corals to build their skeletons), and Arctic species are losing sea ice.

Is it too late to stop climate change?

No. NASA notes that if we stopped adding greenhouse gases, global temperatures would level off within a few years. Some warming is locked in, but every bit of warming we avoid reduces the harm.

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Sources

  1. NASA Science, The Causes of Climate Change
  2. NASA Science, What Is the Greenhouse Effect?
  3. NASA Science, What's the Difference Between Weather and Climate?
  4. NASA Science, Evidence
  5. NASA Science, The Effects of Climate Change
  6. NASA Science, Is It Too Late to Prevent Climate Change?
  7. NASA Earth Observatory, Climate and Earth's Energy Budget
  8. NASA, Carbon Dioxide (Earth Indicator)
  9. NOAA Climate.gov, Climate Change: Atmospheric Carbon Dioxide
  10. NOAA Climate.gov, Climate Change: Global Temperature
  11. NOAA Global Monitoring Laboratory, Trends in Atmospheric Carbon Dioxide (Mauna Loa)
  12. IPCC AR6 Working Group I, Summary for Policymakers
  13. IPCC AR6 Working Group II, Summary for Policymakers
  14. IPCC AR6 Working Group III, Summary for Policymakers