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.
Your turn
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.
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.
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.
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.
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?
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?
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?
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.
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!
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.
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.
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
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.
To understand what changes the climate, follow the energy:
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 IPCC groups global greenhouse gas emissions (2019) by sector:14
| Sector | Share of emissions | Main sources |
|---|---|---|
| Energy supply | 34% | Burning coal, oil and gas for electricity and heat |
| Industry | 24% | Steel, cement, chemicals |
| Farming, forests and land use | 22% | Deforestation, livestock, rice, fertilizer |
| Transport | 15% | Cars, trucks, ships, planes |
| Buildings | 6% | 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
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.
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
Yes. Scientists have checked the other suspects:
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
A degree or so sounds small, but warming a whole planet takes an enormous amount of energy, and the effects add up:
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
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.
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.
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.
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.
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.
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.
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.
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.
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.