| Carbon Dioxide CO2 |
Methane CH4 |
Nitrous Oxide N2O |
Chlorofluorocarbons CFCs |
Tropospheric Ozone O3 |
Carbon Monoxide CO |
Water Vapor H2O |
|
|---|---|---|---|---|---|---|---|
| Greenhouse Role | Heating | Heating | Heating | Heating | Heating | None | Heats in air; cools in clouds |
| Effect on Stratospheric Ozone Layer | Can increase or decrease | Can increase or decrease | Can increase or decrease | Decrease | None | None | Decrease |
| Principal Anthropogenic Sources | Fossil fuels; deforestation | Rice culture; cattle; fossil fuels; biomass burning | Fertilizer; land use conversion | Refrigerants; aerosols; industrial processes | Hydrocarbons (with NOx); biomass burning | Fossil fuels; biomass burning; deforestation | Land conversion; irrigation |
| Principal Natural Sources | Balanced in nature | Wetlands | Soils; tropical forests | None | Hydrocarbons | Hydrocarbon oxidation | Evapo-transpiration |
| Atmospheric Lifetime | 50 - 200 years | 10 years | 150 years | 60 - 100 years | Weeks to months | Months | Days |
| Present Atmospheric Concentration in Parts per Billion by Volume at Surface | 356,000 | 1709 | 310 | CFC-11: 0.28 CFC-12: 0.53 |
20 - 40 | 100 | 3,000 - 6,000 in stratosphere |
| Preindustrial Concentration (1750 - 1800) at Surface | 280,000 | 790 | 288 | 0 | 10 | 40 - 80 | Unknown |
| Annual Rate of Increase (1980s) | 0.5% | 0.9% | 0.3% | 4% | 0.5 - 2.0% | 0.7 - 1.0% | Unknown |
| Relative Contribution to the Anthropogenic Greenhouse Effect | 60% | 15% | 5% | 12% | 8% | None | Unknown |
Mackenzie, F.T. and J.A. Mackenzie (1995) Our changing
planet. Prentice-Hall, Upper Saddle River, NJ, p 288-307.
(After Graedel and Crutzen, 1990, and UCAR/OIES, 1991c.)