Rate of heating
E=S(1-A)piR2
Heat source of global warming
Sunlight, short UV radiation 0.2-0.4 micro meter
Stefan-Boltzmann constant
5.67 x 10-8Wm-2K-4
Venus
Hot due to CO2 rich atmosphere
Mars
Cold due to less CO2
Greenhouse gases
O3, CFCs, CH4, N2O
CO2
Released when fossil fuels burns - industrial revolution 1990, deforestation, CO2 generation unbalanced
Ice cores
Bubbles trapped, previous CO2 levels mirrored temperature changes (isotopic oxygen and ice layer thickness)
Pre-Industrial Revolution
CO2 levels 275ppm