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CH₄

Methane

Methane (CH4) - same molecule, two reportable GWP-100 values. Fossil 29.8 vs non-fossil 27.0 tCO2e per tonne. AR6.
Data layer: MasterBrain v2026.284 · updated 6 Nov 2026

Methane is the second-largest contributor to anthropogenic warming after carbon dioxide — yet most corporate inventories under-report it, mis-classify it, or apply the wrong Global Warming Potential to it.

Get methane right and you fix the most expensive line item in many Scope 1 inventories. Get it wrong and a single line in your CDP submission can be flagged for restatement.

Quick Answer

Methane (CH₄) is a greenhouse gas with an atmospheric lifetime of 11.8 years and an IPCC AR6 100-year GWP of 29.8 for fossil leaks and processes and 27 for other methane, including from burning fuel. It is the second-largest gas in most corporate Scope 1 inventories.

29.8 IPCC AR6 GWP-100 · fossil methane · per tonne CO₂e

Methane at a glance — key properties

Methane is a four-hydrogen, one-carbon molecule (CH₄) with an atmospheric lifetime of 11.8 years per IPCC AR6 — short enough that emission cuts produce measurable atmospheric concentration drops within a decade. Every property below is sourced directly from IPCC AR6 Working Group I, Tables 7.15 and 7.SM.7.

Methane (CH₄) — physical and reporting properties
Property Value Notes
Chemical formula CH₄ One carbon, four hydrogen atoms
CAS number 74-82-8 Single registry identifier for both origin types
Atmospheric lifetime 11.8 yrs Removed via hydroxyl (OH) oxidation to CO₂ + H₂O
GWP-20 (fossil) 82.5 Near-term horizon — most CH₄ still airborne at year 20
GWP-100 (fossil) 29.8 Oil, gas and coal leaks; fossil industrial processes
GWP-100 (biogenic) 27 Burning any fuel; landfill, livestock, rice
GWP-100 (fossil), IPCC corrected 2025 28.1 IPCC errata, 7 Oct 2025 (non-fossil: 25.3). Reporting frameworks still use 29.8. What changed
GWP-500 (fossil) 10 Long horizon — most methane has decomposed by year 500
AR5 GWP-100 (legacy) 28 · outdated Superseded by AR6, which the GHG Protocol and CDP recommend
AR5 → AR6 change (fossil) +6.4% Material for any inventory with sizeable CH₄ exposure
Source table AR6 WGI Table 7.15 Corrected by the IPCC in October 2025; AR7 due ~2028

Source: IPCC AR6 Working Group I, Table 7.15 (fossil and non-fossil methane) and Table 7.SM.7 (2021); corrected values from the IPCC AR6 WGI errata (7 October 2025). For the full AR6 dataset across all Kyoto gases, see the IPCC AR6 GWP reference table.

Methane vs CO₂ — why time horizon decides everything

Methane is often summarised as “X times more potent than CO₂”, but the multiplier depends entirely on the time horizon you choose. For most greenhouse gases, GWP-20 and GWP-100 are similar enough that the choice does not move the inventory total. For methane, the two values differ by a factor of about 2.8 — so the horizon decision is, in practice, a methane decision.

Methane (CH₄) vs Carbon dioxide (CO₂) — radiative and atmospheric behaviour
Property Methane CO₂ Practical implication
Atmospheric lifetime 11.8 yrs 100–300+ yrs Methane acts fast then disappears; CO₂ accumulates for centuries
GWP-20 82.5 1 ~83× CO₂ over 20 years — methane is the fastest near-term lever
GWP-100 (default basis) 29.8 1 Standard horizon for all corporate GHG inventories
GWP-500 10.0 1 Most methane has broken down; CO₂ persists
Radiative efficiency High per molecule Lower per molecule Methane absorbs IR radiation far more efficiently
Climate priority Fastest near-term lever Dominant long-term driver Methane cuts produce observable temperature benefit within a decade
Key insight — the GWP-20 vs GWP-100 decision is a methane decision

For an organisation with significant natural gas combustion or fugitive methane, switching from GWP-100 to GWP-20 reporting raises Scope 1 by a factor of about 2.8 on the methane component — with no change in actual emissions. Always document the horizon used and the reason. The default for almost every corporate framework (GHG Protocol, CSRD, CDP) is GWP-100. See our GWP explainer for the full time-horizon decision tree.

Fossil vs biogenic methane — the AR6 split most inventories miss

IPCC AR6 was the first Assessment Report to publish two separate GWP-100 values for methane depending on its origin. The split is small in absolute terms (1.9 units) but matters for two reasons: it is required for accurate inventories under the GHG Protocol, and it is increasingly checked by external assurance providers and CDP reviewers.

Fossil methane

From hydrocarbons sequestered for millions of years

29.8

GWP-100 (AR6) · Use for fossil methane that escapes unburned: leaks, venting and fossil industrial processes. When it oxidises in the air its fossil carbon becomes new CO₂, which this value includes.

  • Fugitive losses from pipelines, valves, compressors
  • Coal mine ventilation methane
  • Oil well associated gas and venting

Scope 1 — direct emissions

Biogenic methane

From recently living organic matter

27

GWP-100 (AR6) · Use for biological methane and for methane from burning any fuel, including natural gas. The value leaves out the CO₂ the methane later forms, because that carbon is either recent or already counted in the fuel’s combustion CO₂.

  • Landfill gas from organic waste decomposition
  • Livestock enteric fermentation (cattle, sheep)
  • Anaerobic digestion of food and farm waste
  • Rice cultivation (paddy methane)

Scope 1 or Scope 3 Cat 5 by ownership

Which value to use — fossil 29.8 [GreenCalculus gwp.CH4_fossil.ar6_100 · IPCC AR6 · v2026.284] only for leaks and fossil processes

The GHG Protocol GWP values (v2.0, August 2024) keep the fossil value, 29.8 [GreenCalculus gwp.CH4_fossil.ar6_100], for methane from oil and gas systems, coal mining and fossil industrial processes. All other methane uses the non-fossil value, 27 [GreenCalculus gwp.CH4_biogenic.ar6_100 · IPCC AR6], and that includes methane from burning fuel in boilers, engines and vehicles. Combustion CO₂ already counts the fuel’s carbon, so applying the fossil value to combustion methane would count that carbon twice.

Historical note. AR5’s headline CH₄ GWP-100 of 28 [GreenCalculus gwp.CH4_fossil.ar5_100 · IPCC AR5] applied to both origins (AR5 also gave 30 for fossil methane, which DEFRA and the UNFCCC did not adopt). The AR6 split was introduced in 2021 as the science of carbon-cycle accounting matured. The GHG Protocol and CDP recommend AR6, and ESRS E1 calls for the latest IPCC values. AR5 stays in use under some regimes, so state which set you use. See our IPCC AR6 standards page for the full transition timeline.

Where methane shows up across Scope 1, 2, and 3

For a typical corporate reporter — a manufacturer, commercial property operator, agricultural business, or service company with natural gas use — methane appears in four places under the GHG Protocol Corporate Standard. The first three are common to almost every reporter; the fourth is specific to organisations with biogenic sources.

Scope 1
Stationary combustion — natural gas methane slip

When natural gas burns, the overwhelming majority of emissions are CO₂ from the carbon content of the fuel. A small fraction of the CH₄ in the gas, however, does not combust completely — this uncombusted residual is known as methane slip, and it contributes to the Scope 1 total. DEFRA 2025 pre-aggregated CO₂e factors for natural gas already include this slip component, applied at the AR5 GWP-100 (DEFRA’s stated basis). If you are calculating from first principles using separate CO₂, CH₄, and N₂O factors instead, apply the AR6 non-fossil GWP-100 of 27 [GreenCalculus gwp.CH4_biogenic.ar6_100] to the methane mass, as the GHG Protocol does for combustion — never both.

Scope 1
Fugitive emissions — leaks from owned gas infrastructure

Any organisation that owns or operates natural gas pipework, valves, compressors, connectors, or storage has a potential fugitive methane source. These are Scope 1 direct emissions because the leaking equipment is owned or controlled by the reporting entity. Fugitive methane is the most under-reported Scope 1 source in practice — it requires deliberate estimation or measurement rather than meter readings. For organisations with extensive gas networks, fugitives can exceed combustion emissions in warming impact.

Scope 3 Cat 3
Upstream fuel and energy — well-to-tank methane

The natural gas that arrives at your meter came from a well, travelled through a transmission network, and was processed at a terminal — every step of which leaks methane before the gas reaches you. These upstream fugitive emissions are Scope 3 Category 3 (fuel and energy-related activities) under the GHG Protocol. They are calculated using a well-to-tank emission factor and reported separately from Scope 1 combustion. Many organisations omit them entirely — a significant completeness gap given that upstream methane intensity for some gas sources exceeds 1% of throughput.

Scope 3 Cat 5
Waste — landfill methane from operational waste

Operational waste sent to landfill generates biogenic methane as the organic fraction decomposes anaerobically. This is Scope 3 Category 5 (waste generated in operations) where the waste is sent to a third-party landfill, or Scope 1 where the organisation owns and operates the landfill. Apply the biogenic GWP-100 of 27 [GreenCalculus gwp.CH4_biogenic.ar6_100] to the methane mass calculated from the organic fraction and the landfill-specific decay constant.

Leaks get 29.8 [GreenCalculus gwp.CH4_fossil.ar6_100]; combustion slip gets 27 [GreenCalculus gwp.CH4_biogenic.ar6_100]

Scope 1 fugitives and Scope 3 upstream methane from oil, gas and coal take the fossil AR6 GWP-100 of 29.8 [GreenCalculus gwp.CH4_fossil.ar6_100]. Methane slip from combustion takes the non-fossil 27 [GreenCalculus gwp.CH4_biogenic.ar6_100]. The Scope 1 Combustion Calculator applies this automatically — the audit trail shows the exact CH₄ mass, the GWP-100 factor, and the resulting CO₂e contribution for every fuel type, alongside an AR5 reconciliation column.

Converting methane mass to CO₂-equivalent

The conversion from methane mass to CO₂-equivalent is a single multiplication. The structure is identical for every source — combustion slip, fugitive, upstream, or biogenic — provided you select the GWP that matches the origin type.

tCO₂e = tonnes CH₄ × GWP-100
Natural gas boiler — methane slip (combustion, AR6 non-fossil)
0.5 t CH₄ × 27
= 13.5 tCO₂e
Pipeline fugitive leak (fossil, AR6)
2 t CH₄ × 29.8
= 59.6 tCO₂e
Landfill gas from operational waste (biogenic, AR6)
10 t CH₄ × 27
= 279 tCO₂e
Same fossil leak under outdated AR5 basis
2 t CH₄ × 28
= 56.0 tCO₂e

The Scope 1 Combustion Calculator handles this conversion automatically for natural gas, biogas, and other methane-bearing fuels. It applies the correct AR6 GWP, shows the methane mass derived from the fuel input, and produces a downloadable audit trail aligned with assurance requirements.

Calculate methane emissions in seconds, with a verifier-ready audit trail.

The Scope 1 Combustion Calculator applies AR6 CH₄ GWP-100 = 27 [GreenCalculus gwp.CH4_biogenic.ar6_100] (non-fossil, the GHG Protocol value for combustion) automatically across all fossil and biofuels, with a per-gas breakdown and AR5/AR6 reconciliation column.

Regulatory landscape — methane is now disclosed, taxed, or both

Methane regulation has moved from voluntary to enforceable across most major jurisdictions in the past three years. Reporters with material methane exposure should track these four regimes.

Major methane regulatory regimes — status May 2026
Jurisdiction Regime Scope Status
EU Methane Emissions Regulation 2024/1787 (MERR) Oil, gas, coal — production and imports. LDAR programmes, venting/flaring restrictions, methane intensity limits In force from 4 Aug 2024. Routine flaring/venting prohibition from 5 Feb 2026. Import equivalence from 1 Jan 2027. Maximum methane intensity from 5 Aug 2030
EU CSRD / ESRS E1 All in-scope companies — methane reported as part of disaggregated GHG disclosure (E1-6) In force. AR6 GWP-100 required
US EPA NSPS OOOOb / EG OOOOc Oil and gas — new and existing source methane standards. Super-emitter response programme Final rule March 2024. Subject to ongoing reconsideration; certain compliance deadlines extended in 2025–2026
US GHGRP Subpart W Petroleum and natural gas systems — facility-level methane reporting, >25,000 t CO₂e/yr In force. Empirical-data revisions effective from reporting year 2025
Global CDP Climate Change disclosure All voluntary corporate disclosure AR6 GWP-100 mandatory from 2023 reporting cycle
Global OGMP 2.0 Voluntary oil and gas — Level 5 measurement-based methane reporting De facto benchmark for EU MERR import equivalence
Compliance trap — the AR5 to AR6 transition is asynchronous

Frameworks treat AR6 GWP-100 differently: the GHG Protocol and CDP recommend it, and ESRS E1 calls for the latest IPCC values. DEFRA pre-aggregated UK conversion factors still use the AR5 basis as of the 2025 release. Reporters with multi-jurisdictional disclosure obligations need to know which factor basis applies to which submission, and document the choice in the methodology appendix. The Scope 1 Combustion Calculator exposes both bases in parallel for exactly this reason.

Five methane-specific mistakes auditors flag

01
Omitting fugitive methane entirely. Combustion shows up automatically in meter readings; fugitives do not — they require a deliberate estimation or measurement programme. Inventories that include natural gas combustion but carry no fugitive line are common, and assurance providers flag them as completeness failures under the GHG Protocol. A conservative estimate using industry-average leak rates is better than zero, and is acceptable as an interim approach pending a proper LDAR programme.
02
Using the AR5 GWP of 28 [GreenCalculus gwp.CH4_fossil.ar5_100] when AR6 29.8 [GreenCalculus gwp.CH4_fossil.ar6_100] applies. The 6.4% increase compounds across every tonne of CH₄ in the inventory. For a manufacturer consuming 50 million m³ of natural gas annually, the methane slip component alone can represent several hundred tonnes of CO₂e — and the AR5/AR6 gap on that methane is material. CDP reviewers have flagged this consistently from the 2023 reporting cycle onwards. CSRD-scope reporters must use AR6.
03
Applying the fossil GWP to confirmed biogenic methane (or vice versa). If your organisation operates a landfill, anaerobic digester, or livestock facility and can document biogenic origin, use 27 [GreenCalculus gwp.CH4_biogenic.ar6_100] rather than 29.8 [GreenCalculus gwp.CH4_fossil.ar6_100]. The 2.8-unit gap is small per tonne but becomes numerically significant at scale, and the discipline of using the right factor matters for auditability. The reverse error — applying the non-fossil value to fossil leaks or venting — is more serious because it understates emissions. Combustion methane is the exception: there the non-fossil value is correct.
04
Double-counting methane in pre-aggregated CO₂e factors. DEFRA 2025 natural gas factors are published in kg CO₂e per kWh — already incorporating CH₄ and N₂O components at AR5 GWP. If you use these factors, do not add a separate methane calculation on top: that double-counts. Calculate methane independently only when working from raw gas composition data or first-principles combustion equations, and apply AR6 GWP at that point. The two methods produce slightly different totals (because of the AR5 vs AR6 GWP shift); both are correct disclosures of distinct methodologies, but mixing them is not.
05
Mixing GWP-20 and GWP-100 within one inventory. A small but recurring error: applying GWP-20 to methane (because of the fast-acting framing in climate communications) while applying GWP-100 to N₂O and the F-gases. IPCC AR6 explicitly warns against this — choose one time horizon and apply it consistently across every gas. GWP-100 is the corporate default. GWP-20 is appropriate only for short-lived climate pollutant analysis or where a specific framework requires it.

Need methane done right across your full inventory?

The GreenCalculus calculator suite covers Scope 1 combustion, Scope 1 fugitives, Scope 3 upstream fuel emissions, and refrigerant leakage — all using the latest IPCC AR6 GWP basis with full audit trails for assurance.

Methane (CH₄) explained — IPCC AR6 GWP-100 of 29.8 (fossil) and 27 (biogenic).
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Frequently asked questions

The IPCC AR6 GWP-100 for fossil methane is 29.8 [GreenCalculus gwp.CH4_fossil.ar6_100], from WGI Table 7.15 as published in 2021 (the IPCC corrected it to 28.1 [GreenCalculus gwp.CH4_fossil.ar6e_100 · IPCC AR6 2025] in October 2025; reporting frameworks have not yet adopted the correction). This is the value for oil and gas fugitive emissions, coal-mine methane and fossil industrial processes. For methane from burning any fuel, and for biogenic methane — landfill, livestock, rice cultivation — the AR6 GWP-100 is 27 [GreenCalculus gwp.CH4_biogenic.ar6_100]. The earlier AR5 value of 28 [GreenCalculus gwp.CH4_fossil.ar5_100] is outdated for current corporate reporting; CDP recommends AR6 and CSRD calls for the latest IPCC values.

Methane absorbs infrared radiation far more efficiently than CO₂ per molecule, and because most of it is still airborne at year 20, its GWP-20 (fossil) is 82.5 [GreenCalculus gwp.CH4_fossil.ar6_20 · IPCC AR6] — roughly 83 times that of CO₂ over the same period. This makes methane reduction the fastest near-term lever for slowing warming. The reason GWP-100 (29.8 [GreenCalculus gwp.CH4_fossil.ar6_100]) is lower is simply that we are averaging over a longer period: by year 12–15 most of the methane has been oxidised to CO₂, so the cumulative 100-year impact per tonne is proportionally smaller.

Methane has a perturbation lifetime of approximately 11.8 years per IPCC AR6. It is removed from the atmosphere primarily through reaction with hydroxyl radicals (OH) in the troposphere, which oxidises it into CO₂ and water vapour. This is fundamentally different from CO₂, which has no equivalent removal sink and persists in the atmosphere for 100 to 300+ years. The short methane lifetime means that emission cuts produce measurable atmospheric concentration drops within a decade — unlike CO₂, where the benefit accumulates over centuries.

Fossil methane (GWP-100 = 29.8 [GreenCalculus gwp.CH4_fossil.ar6_100]) comes from underground hydrocarbon deposits — natural gas, oil wells, coal seams. Every tonne released is a net addition of ancient carbon to the active atmosphere. Biogenic methane (GWP-100 = 27 [GreenCalculus gwp.CH4_biogenic.ar6_100]) comes from biological processes involving recently living organic matter — livestock digestion, landfill decomposition, wetlands, rice paddies. IPCC AR6 introduced separate GWPs for the two origins. For corporate GHG Protocol reporting, use 29.8 [GreenCalculus gwp.CH4_fossil.ar6_100] for fossil fugitive and fossil process sources, and 27 [GreenCalculus gwp.CH4_biogenic.ar6_100] for combustion of any fuel and for biogenic sources.

For a typical reporter, methane appears in four places. First, as Scope 1 combustion methane slip — uncombusted CH₄ in natural gas. Second, as Scope 1 fugitive emissions from any natural gas pipework, valves, or equipment the organisation owns or controls. Third, as Scope 3 Category 3 (fuel and energy-related activities) — upstream methane lost during the extraction, processing, and transmission of the gas purchased. Fourth, as Scope 3 Category 5 biogenic landfill methane from operational waste sent to third-party disposal. Pre-aggregated DEFRA factors include the combustion slip automatically (at AR5 GWP); the other three sources require separate calculation.

For almost every current corporate framework — GHG Protocol Corporate Standard, CSRD/ESRS E1, CDP — the answer is AR6. The AR5 fossil CH₄ GWP-100 of 28 [GreenCalculus gwp.CH4_fossil.ar5_100] is retained only for legacy comparisons and base-year restatement; it should not be used for new reporting. The exception is when working with pre-aggregated DEFRA UK conversion factors, which are themselves published on the AR5 basis — in that case, the factor is internally consistent with AR5 and you should not separately apply AR6 GWP on top. The Scope 1 Combustion Calculator exposes both bases and reconciles them in the audit trail.

Primary source. Forster, P. et al. (2021). The Earth’s Energy Budget, Climate Feedbacks and Climate Sensitivity — Supplementary Material. In Climate Change 2021: The Physical Science Basis (IPCC AR6 WGI). Cambridge University Press. Table 7.SM.7, p.7-SM-47. ipcc.ch/report/ar6/wg1/

GWP values cited. Fossil CH₄ GWP-100 = 29.8 (AR6). Non-fossil (biogenic and combustion) CH₄ GWP-100 = 27.0 (AR6). AR5 CH₄ GWP-100 = 28.0 (legacy). Methane atmospheric lifetime = 11.8 yr. GWP-20 fossil = 82.5. GWP-500 fossil = 10. AR6 values are from WGI Table 7.15 and already include the carbon-cycle response (AR6 publishes one set, not a with/without pair). The IPCC errata of 7 October 2025 correct fossil / non-fossil GWP-100 to 28.1 / 25.3. Values re-checked against Table 7.15 and the errata by Jeremiah Say, 15 October 2026.

Regulatory references. Regulation (EU) 2024/1787 on the reduction of methane emissions in the energy sector (in force 4 Aug 2024). 40 CFR Part 60 Subpart OOOOb / OOOOc (US EPA, March 2024, in reconsideration). 40 CFR Part 98 Subpart W (US EPA GHGRP). CSRD Directive (EU) 2022/2464 with ESRS E1 disclosures.

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