Climate impact is more than CO₂

The Science and Impact of Non-CO₂ Aviation Emissions

Aviation warming is driven not only by long-lived CO₂, but also by short-lived, high-intensity effects: contrails/contrail cirrus, soot (nvPM), SOx-derived aerosols, and NOx chemistry. The lever is fuel chemistry.

Short-term climate leverage Because non-CO₂ effects last hours to days, reducing their precursors can cut radiative forcing quickly.
≈ 66%
Share of total warming
Non-CO₂ effects represent roughly two-thirds of aviation’s warming impact.
Hours → Days
Persistence
Short-lived atmospheric effects: rapid payoff if precursors are removed.
Fuel chemistry
Primary lever
Aromatics (esp. naphthalene) and sulfur drive soot and aerosols that seed contrails.

1) The Aviation Emission Spectrum: CO₂ vs. Non-CO₂

Persistence • Share • Culprits • Mitigation

Aviation’s climate footprint (at a glance)

CO₂ persists for centuries, while non-CO₂ effects are short-lived but dominate near-term warming.

Key climate impact drivers

Contrail cirrus, nvPM soot, SOx, and NOx chemistry.

FeatureCO₂ EffectsNon-CO₂ Effects
PersistenceCenturies.Hours to days.
Share of Total Impact~1/3.~2/3 (≈66%).
Primary CulpritsTotal carbon.Aromatics, naphthalene, sulfur.
Mitigation FocusLifecycle carbon + efficiency.Fuel chemistry + strategic routing.

2) The Physics of the Exhaust: From Aromatics to Ice

Chemical logic flow

Chemistry → particles → clouds

Polycyclic aromatics (notably naphthalene) form soot that seeds ice crystals in cold, humid cruise conditions.

Practical takeaway

Contrail persistence is strongly influenced by soot particle density, linked back to aromatic fraction.

3) Quantifying the Impact: Dominance of Non-CO₂ Effects

NRFGWP 20/50/100

Net Radiative Forcing (NRF)

NRF captures the net imbalance in radiation; contrail-induced cloudiness is a major driver.

Short-lived leverage

Reduce precursors and you reduce warming quickly (hours to days), unlike CO₂.

Impact split (illustrative)

Approximate share of warming: CO₂ (~1/3) vs non-CO₂ (~2/3).

Near-term “cooling opportunity”

Immediate payoff Fewer soot/aerosol precursors → fewer ice nuclei → less contrail forcing (when conditions allow).

4) Regulatory Phase Shift: Regulation (EU) 2024/2493

MRVNEATSDefault values

From voluntary to legal compliance

Non-CO₂ effects are moving into mandatory monitoring and reporting; fuel chemistry becomes compliance-critical.

NEATS

Weather-based modelling estimates CO₂e per flight. Missing chemistry data can trigger “worst-case” defaults.

Monitoring mandate timeline

Jan 1, 2025 — Monitoring mandate begins
Start

Airlines track and monitor non-CO₂ effects per flight.

Mar 31, 2026 — First verified reporting deadline
Verified

Reported data on soot, aromatics, sulfur becomes visible to regulators.

Future — Integration into pricing mechanisms
ETS

High-aromatic/high-sulfur fuels may face financial penalties.

Default values (worst-case inputs)

25% aromatics (vol)Incentivizes verified low-aromatic profiles.
0.3% sulfur (mass)Higher sulfur drives SOx and sulfate aerosol effects.
3.0% naphthalene (vol)Polycyclic aromatics strongly link to soot formation.

Compare your fuel vs default values

Leave blank to simulate “missing data”.

Default: 25.0
Default: 0.300
Default: 3.0
Enter values to evaluate.
Defaults shown reflect the stated “worst-case” inputs. Blank fields simulate “missing data”.

5) Technical Gap: Why SAF Isn’t a Near-Term Cure-All

CostSupplyBlend wall

The SAF reality check

Economics, supply constraints, and blend limits restrict how quickly SAF can remove soot precursors at scale.

The blend wall

Many SAF streams lack aromatics; legacy sealing requirements impose blending limits, retaining fossil fractions.

ConstraintData PointConsequence
Economice-SAF ~13×; Bio-SAF ~3–5× vs fossil jetBarrier to wide adoption.
Supply~1.6% of global demandShortfall vs mandates.
Technical50% blend limit (ASTM D7566)Fossil fraction remains → precursors persist.

6) Empirical Evidence: TERC Test Results

nvPM reductionSulfur < 10 ppm

Headline results

Aromatics ~8.5% (vs ~18–25%). Full load particle number down ~40–50%, mass down ~30–40%. Sulfur down ~99.7% to <10 ppm.

Why it matters

Fewer particles → fewer ice nuclei → potential for thinner/shorter-lived contrails under suitable conditions.

Illustrative reductions (midpoints)

Midpoints: Full load (number 45%, mass 35%); Idle (number 35%).

Quick reference

Aromatics profileJet A-1 ~18–25% vs ~8.5%.
Sulfur reduction~99.7% to <10 ppm (SOx nearly eliminated).

7) Summary of Insights

Commodity → technologyCompliance infrastructure

From commodity to technology

Fuel chemistry (soot/sulfur/aromatics) becomes measurable climate and compliance performance.

Compliance enabler

Low-aromatic, low-sulfur fuels can help avoid punitive defaults under MRV regimes.

The scientific imperativeUnderstanding high-altitude cloud physics enables near-term radiative forcing reduction.
Caveats & positioning guardrails
tLCAF / zLCAF are positioned as drop-in Jet A-1 with a QA + traceability evidence pack. Any MRV interpretation remains airline-controlled and verifier-led.