Every time you ride in a gas-powered car, eat a hamburger or toss food scraps in the garbage, greenhouse gases end up in the air. But plants, soils and oceans are pulling some of those gases back out at the same time. Whether the amount in the atmosphere rises or falls depends on the balance between sources, which release a gas, and sinks, which remove and store it. Right now, human activity has tipped the balance so that sources outrun sinks.
The main greenhouse gases
| Gas | Natural sources | Human sources | Sinks and removal |
|---|---|---|---|
| Carbon dioxide, CO₂ | Respiration, decomposition, volcanoes, wildfires, release from warm ocean water | Burning coal, oil and natural gas; cement making; clearing and burning forests | Photosynthesis (forests, peatlands, soils); dissolving in the ocean; very slow rock weathering. Part of any added CO₂ stays in the air for centuries or longer |
| Methane, CH₄ | Wetlands, termites, thawing permafrost | Livestock digestion (especially cattle), landfills, rice paddies, leaks from natural gas, oil and coal production | Breaks down by chemical reactions in the atmosphere in about a decade |
| Nitrous oxide, N₂O | Bacteria in soils and oceans | Nitrogen fertilizers and manure, some industrial processes, burning fuels | Broken down slowly by ultraviolet light in the stratosphere, over about a century |
| Halocarbons (CFCs, HCFCs, HFCs) | Almost none: nearly all are human-made | Refrigerants in fridges and air conditioners, aerosol propellants, foams, solvents | Broken down very slowly by ultraviolet light in the stratosphere; some last for centuries |
| Water vapour, H₂O | Evaporation from oceans and lakes, transpiration from plants | Very little directly | Condensation and precipitation, within about a week or two |
Comparing gases: global warming potential
Tonne for tonne, some gases trap far more heat than CO₂. Global warming potential (GWP) compares the warming caused by 1 tonne of a gas over 100 years with the warming caused by 1 tonne of CO₂, which is defined as GWP = 1. Methane's GWP is about 28, nitrous oxide's about 270, and some halocarbons have GWPs in the thousands. To add up different gases, scientists convert each one to carbon dioxide equivalent (CO₂e). CO₂ still causes most of the human-caused warming, because we release so much more of it and much of it stays in the air for a very long time.
The carbon cycle and the global carbon budget
Carbon moves among reservoirs: the atmosphere (as CO₂ and CH₄), living things, soils and peat, the oceans (as dissolved CO₂ and carbonate), and rocks and fossil fuels. In the fast carbon cycle, carbon moves between air, living things and the surface ocean over years to centuries through photosynthesis, respiration, decomposition and gas exchange. In the slow carbon cycle, carbon moves into and out of rocks over millions of years, through volcanoes and the weathering of rock. Fossil fuels are carbon that plants and plankton removed from the air millions of years ago. Burning them moves carbon from the slow cycle into the fast cycle in decades.
- Fossil fuels released a record of about 38 billion tonnes of CO₂ in 2025, according to the Global Carbon Project; land-use change (mostly deforestation) added several billion tonnes more.
- Over the past decade, roughly half of human CO₂ emissions stayed in the atmosphere, about a quarter to a third dissolved into the oceans, and about a fifth to a quarter was taken up by plants and soils on land.
- The ocean sink has a cost: dissolved CO₂ forms carbonic acid, so ocean water is becoming more acidic (ocean acidification), which harms shell-building organisms such as corals, oysters and some plankton.
- Sinks can weaken: hot, dry years and wildfires reduce how much carbon forests absorb, and thawing permafrost can turn a carbon store into a source.
Human factors and Canada's contribution
The main human factors that add greenhouse gases are burning fossil fuels for transportation, heating and electricity; industrial emissions from making cement, steel, chemicals and fertilizer and from extracting oil and gas; deforestation, which both releases stored carbon and removes a sink; and forest fires, which release CO₂ quickly (fires have natural causes too, but people start many of them, and a warmer climate makes large fires more likely). Agriculture adds methane and nitrous oxide.
| Canada's emissions (2023 national inventory) | Value |
|---|---|
| Total greenhouse gas emissions | About 694 million tonnes CO₂e |
| Change since 2005 | About 8.5% lower |
| Share of world emissions | About 1.5% |
| Per person | About 17 tonnes CO₂e, well over twice the world average |
| Largest sector | Oil and gas production, about 30% (208 Mt) |
| Second-largest sector | Transportation, about a fifth |