Introduction to Greenhouse Gas Emissions from Aviation
There are four main ways that aviation emissions affect climate, each of which is described in more detail:
Direct emissions of Greenhouse Gases (GHGs): notably carbon dioxide (CO2) and water vapor (H2O)- Indirect impacts on GHGs: non-GHGs or weak GHGs such as nitrogen oxides (NOx) catalyze changes in concentrations of other GHGs such as ozone (O3) and methane (CH4)
- Emissions of aerosols: emissions of particulates that have cooling or warming effects such as sulfates and soot
- Formation of contrails and cirrus clouds
These emissions occur in the troposphere and lower stratosphere. The troposphere is the lowest part of Earth's atmosphere and its height extends to altitudes between 8 and 15km. The stratosphere lies between the troposphere and the mesosphere. It starts at an altitude of 8 to 15km and extends to 50 km.
Summary of Climatic Response to Aircraft Emissions:
CO2 |
NOx Ozone increase |
NOx Methanedecrease |
NOx Ozone decrease |
Aerosols (particulates) |
Contrails and Cirrus Clouds |
|
Mean temperature response |
warming |
warming |
cooling |
cooling |
warming (soot) and cooling (sulfates) |
Net warming |
Duration on the order of |
centuries |
weeks to months |
decade |
decade |
days to weeks |
contrails: hours aviation-induced cirrus: hours - days |
Spatial distribution |
global |
continental to global |
continental to global |
continental to global |
soot: sulfates: continental to global |
local to continental |
Scientific understanding (Scale: good - fair - poor) |
good |
fair |
fair |
fair |
fair |
poor |