Climate

The bigger part of aviation's warming

CO2 is not the only way flying warms the planet. The white lines behind aircraft can spread into cirrus cloud that traps heat. On the reference assessment, that effect is larger than the warming from aviation's CO2.

The numbers

57%Of aviation's net warming effect from contrail cirrus2018 · effective radiative forcing · best estimate, low confidence · Lee et al. 2021
~3×Aviation warms at about three times the rate of its CO2 aloneLee et al. 2021
2%Of flights caused 80% of contrail energy forcing2019 · Teoh et al. 2024
24%Of flights formed a persistent contrail2019 · Teoh et al. 2024
2025EU monitoring of non-CO2 effects began1 January 2025 · Directive (EU) 2023/958
2027Commission report, and proposals where appropriateBy 31 December 2027 · Directive (EU) 2023/958
At any given moment, contrails trap more heat than all the CO2 aviation has emitted since 1940.Lee et al. 2021: contrail cirrus 57.4 mW/m² against 34.3 mW/m² from all aviation CO2 accumulated since 1940 (2018).

Contrail science is uncertain, and the authors rate their confidence in the contrail term as low. On a CirculAIRity Monte Carlo of Lee et al.'s own uncertainty ranges, the contrail share lies between 27% and 73% (5–95%). We show ranges, never a single heroic number.

How a contrail forms

Ice on soot

A contrail forms when hot, humid exhaust mixes with cold air and briefly reaches water saturation. Water condenses on particles in the plume, mainly engine soot, and freezes into ice crystals. Most contrails vanish within minutes; in ice-supersaturated air they persist and spread into cirrus that can last for hours. Kärcher 2018

Why it warms

Trapping heat, day and night

By day a contrail reflects sunlight, which cools. Day and night it traps heat from the surface, which warms. On the global average the warming wins, and night-time and winter contrails warm the most. Fewer, larger ice crystals make a thinner, shorter-lived contrail. Kärcher 2018; Burkhardt et al. 2018

Avoidance

Rerouting helps some flights. It cannot reach most.

Contrail avoidance changes a flight's time, altitude or path so it misses the air most likely to form warming contrails. It works when the right flights can be moved and the forecast is right.

What works
  • A 2021 night-time live trial at Maastricht avoided contrails by moving flights ±2,000 ft. EUROCONTROL MUAC 2024
  • A 2023 airline trial saw 63.6% fewer contrails on flights given avoidance guidance, against a control group. Sanekommu et al. 2024
The limits
  • Short-term forecasts of ice-supersaturated air remain poor. Gierens et al. 2020; Hofer, Gierens and Rohs 2024
  • In simulation, blocking flight levels for avoidance cut sector capacity by at least 20%. EUROCONTROL MUAC 2024
  • Every diversion burns extra fuel: a certain CO2 cost against an uncertain contrail benefit.
  • The largest planned European avoidance programme would reach about 0.04–0.05% of annual European flights. CirculAIRity calculation: about 4,500 flights a year (Blue Lines 2024, citing Aviation Week) ÷ 10.69 million flights in 2024 (EUROCONTROL 2025)
One unit for all of aviation's warming

Tonnes of CO2-warming-equivalent

tCO2-WE expresses any emission or effect as the tonnes of CO2 that would cause the same change in global temperature. It comes from the GWP* method developed at the University of Oxford, and it is the basis on which the reference assessment reports aviation's warming. Allen et al. 2018; Cain et al. 2019; Lynch et al. 2020; Lee et al. 2021

MetricWhat it measuresHow it treats contrailsUsed by
GWP100 (tCO2e)Heat trapped over 100 years after a one-off releaseA year of contrails counts as a short pulse spread over a centuryUNFCCC reporting; EU and UK ETS; CORSIA
GWP20Heat trapped over 20 years after a one-off releaseCounts contrails heavily; the 20-year horizon is arbitrarySome short-term climate studies
GTP100Temperature 100 years after a one-off releaseCounts almost nothing: the warming has long goneSome IPCC comparisons
GWP* (tCO2-WE)The temperature effect of a change in emission rateCounts a sustained cut in contrails as the CO2 removal that would cool the planet as muchLee et al. 2021; CirculAIRity
5.3tCO2-WE of contrail warming per tonne of fuelGWP*, 30-year period
1.9tCO2e per tonne of fuelGWP100

The same year of contrails is 1.9 tCO2e per tonne of fuel on GWP100, and 5.3 tCO2-WE over a 30-year period on GWP*. The period matters: about 7.6 over 20 years, 3.3 over 50 and 1.9 over 100.

CirculAIRity calculation from Lee et al. inputs (contrail cirrus 57.4 mW/m²; 327 Mt of fuel in 2018; α = 0.25, H = 100 years per Cain et al.). Lee et al.'s own Table 5 gives about 5.6, 2.0 and 7.3 per tonne on GWP*, GWP100 and GWP20, which corroborates it.

Our standard: every result in tCO2-WE by GWP*, over a declared 30-year period, with GWP100 and GWP20 alongside.

Regulating and deciding

Both units are right

Regulators count in tCO2e: it is the legal unit under the Paris Agreement, and the EU's non-CO2 monitoring converts each flight's effects using GWP20, GWP50 and GWP100. GWP* has been criticised for favouring established emitters, and we say so. Rogelj and Schleussner 2019

But the question that matters for a contrail measure is how much warming it avoids, and that is what tCO2-WE measures. The IPCC recognises the difference and recommends no single metric: the choice depends on the question. IPCC 2021, AR6 WG1

In short

tCO2e is right for accounting and compliance. tCO2-WE is more right for the question that matters: how much warming is avoided. We report both and decide on tCO2-WE.