B.2.2 emissivity as the ratio of the power radiated per unit area by a surface compared to that of an ideal power radiated per unit area black surface at the same temperature as given by emissivity = σT 4
B.2.3 albedo as a measure of the average energy reflected off a macroscopic system as given by total scattered power albedo = total incident power
B.2.4 that Earth’s albedo varies daily and is dependent on cloud formations and latitude
B.2.5 the solar constant S
B.2.6 that the incoming radiative power is dependent on the projected surface of a planet along the S direction of the path of the rays, resulting in a mean value of the incoming intensity being 4
B.2.7 that methane CH4, water vapour H2O, carbon dioxide CO2, and nitrous oxide N2O, are the main greenhouse gases and each of these has origins that are both natural and created by human activity
B.2.8 the absorption of infrared radiation by the main greenhouse gases in terms of the molecular energy levels and the subsequent emission of radiation in all directions
B.2.9 that the greenhouse effect can be explained in terms of both a resonance model and molecular energy levels
B.2.10 that the augmentation of the greenhouse effect due to human activities is known as the enhanced greenhouse effect.
All content on this website has been developed independently from and is not endorsed by the International Baccalaureate Organization. International Baccalaureate and IB are registered trademarks owned by the International Baccalaureate Organization.