GWP is the unit that lets us compare the climate impact of different greenhouse gases on a single scale. This guide explains what it is, how it's calculated, and the values most often used in carbon inventories.
Global Warming Potential measures how much energy the emissions of 1 tonne of a gas will absorb over a given time period, relative to the emissions of 1 tonne of carbon dioxide. The most commonly used time horizon is 100 years (GWP₁₀₀).
Reporting frameworks — including the GHG Protocol, ISO 14064 and Australia's NGER scheme — use GWP values to convert emissions of all greenhouse gases into a single "carbon dioxide equivalent" (CO₂e) figure.
GWP combines two factors: the radiative efficiency of a gas (how strongly it traps heat per molecule) and its atmospheric lifetime (how long it persists before breaking down). Methane, for example, is far more potent than CO₂ per molecule but lifts out of the atmosphere within a decade or two — which is why its GWP₂₀ value is much higher than its GWP₁₀₀ value.
| Gas | Formula | GWP₁₀₀ | Notes |
|---|---|---|---|
| Carbon dioxide | CO₂ | 1 | The reference gas — every other GWP is expressed relative to CO₂. |
| Methane (fossil) | CH₄ | 29.8 | Short-lived but very potent over a 20-year horizon (GWP₂₀ ≈ 82.5). |
| Nitrous oxide | N₂O | 273 | Long-lived; significant from agriculture and combustion. |
| HFC-134a | CH₂FCF₃ | 1,530 | Common refrigerant; being phased down under the Kigali Amendment. |
| Sulphur hexafluoride | SF₆ | 25,200 | Used in electrical switchgear; one of the most potent GHGs known. |
Source: IPCC Sixth Assessment Report (AR6), Working Group I, Chapter 7.
GWP values determine how non-CO₂ emissions show up in your inventory totals. Choosing the right vintage (AR5 vs AR6) and the right time horizon (20 vs 100 years) can materially shift methane- and refrigerant- heavy footprints. Disclosure frameworks usually specify which vintage to use — confirm before you report.