Methane · 5 min read

Why methane. Why now.

Why cut methane now? The 20-year warming clock

Methane warms hard and lasts roughly a decade in the atmosphere. Cut it now, keep it cut, and near-term warming responds. Delay spends that advantage.

Cut methane now because it runs on a short clock. According to the IPCC and UNEP, methane warms about 80 times as much as CO₂ over 20 years, mass for mass, and stays in the atmosphere for roughly a decade. Cuts made this decade slow warming within years you will live through.

Methane rarely gets the lead role in the climate conversation. CO₂ takes the headlines, the charts and most of the guilt. The main component of natural gas, the fuel behind the blue ring on a kitchen hob, gets a walk-on part. Over the next 20 years, that casting is wrong.

How long does methane stay in the atmosphere?

About 12 years, in the IPCC’s assessment, with chemical reactions doing most of the removal. That number is a statistical lifetime. The molecules do not leave together at a fixed hour, like a coach party.

A portion of every CO₂ emission keeps its influence for centuries, which leaves methane as the part of the problem with the shorter memory.

That short stay explains why the multiplier depends on the horizon. Global warming potential adds up a gas’s warming over a chosen period after release. The IPCC puts methane at about 80 times CO₂ over 20 years and about 30 times over 100 years, because by the end of a century the methane has long gone and a share of the CO₂ remains.

Quote the 80 without its 20 years and you have misquoted the science. The same tonne of methane converts into a much larger CO₂e figure under the 20-year metric, and many greenhouse-gas inventories report on the 100-year horizon, so a 20-year value cannot be compared directly with a 100-year total. A CO₂e number should name its metric, its time horizon and the assessment it comes from.

Methane is often grouped with black carbon and some hydrofluorocarbons as a short-lived climate pollutant, and called a super-pollutant because its warming influence per unit mass is high over 20 years. Neither label gives a precise potency, and no multiplier tells you whether one methane project beats another.

A tap left running

The IEA attributes about 30% of the rise in global temperatures since the Industrial Revolution to methane. A short-lived gas holds that share because fresh releases replace what the air removes.

Picture a bath with the plug out and the tap running. The level stays up only while water pours in. Turn the tap down, keep it down, and within a few years the waterline sits lower. CO₂ fills a second bath, one with a far slower drain.

UNEP’s Global Methane Assessment (2021) found that cutting human-caused methane by 45% this decade would avoid nearly 0.3°C of warming by the 2040s. The decade in question is this one, and more than half of it has gone.

Delay has a cruel arithmetic here. Postpone a cut by five years and you postpone its benefit by five years, while the methane released in the meantime warms on schedule.

The Paris Agreement pursues efforts to limit warming to 1.5°C. Against that goal, the nearly 0.3°C in UNEP’s assessment is a serious amount of heat to leave in the air.

Where does methane come from?

Fossil fuel production, agriculture and waste management are the major human source groups. Wetlands release methane too, but natural sources sit outside human-caused inventories. In oil and gas, methane escapes through leaks and through equipment designed to discharge it, and operators may vent gas during maintenance. A controlled release is still an emission.

The IEA identifies established options for fossil fuel operations, including repairing leaks and changing equipment that releases gas. A leak detection and repair programme pairs surveys with maintenance records and follow-up measurements, because finding a leak is only the first step. Somebody still has to fix it and check that the fix held. A single malfunction can turn one site into a super-emitter, with a plume strong enough for remote sensors to detect.

Waste runs on its own timetable. Buried food waste breaks down without oxygen, and a closed landfill can go on producing methane for decades after the last bin lorry has left. Diverting food waste from landfill in the first place remains important, whatever happens to the gas from what is already buried. Agriculture adds livestock digestion, with practical constraints of its own. A biological origin does not make any of that methane harmless.

No universal installation solves every methane problem. The useful question is whether a particular intervention can prevent a release, operate reliably and demonstrate a benefit against a defensible alternative. Location, maintenance and measurement shape the answer.

Does cutting methane replace cutting CO₂?

No. Cumulative carbon dioxide largely determines long-term warming, so deep CO₂ reductions remain necessary whatever happens to methane. Methane cuts bend the near-term curve. CO₂ cuts decide where warming ends up.

Back in the bathroom, methane is the tap you can turn down now. The slow CO₂ drain still needs dealing with, and a credible climate programme keeps both timescales in view.

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Questions this piece answers

Asked and answered.

How much stronger is methane than CO₂?

About 80 times stronger over the 20 years after release, comparing equal masses, according to UNEP. That multiplier belongs to the 20-year horizon. Methane is removed from the atmosphere over roughly a decade, so the figure falls on longer horizons, and every honest comparison names the period it uses.

Why is cutting methane urgent?

Because methane is removed from the atmosphere over roughly a decade, sustained cuts can slow warming in the near term. Deep CO₂ reductions remain necessary, since cumulative carbon dioxide largely sets long-term warming. The IEA lists established options for fossil fuel operations, such as repairing leaks and replacing equipment that releases gas.

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