Soot particles ("black carbon aerosols") cause warming by absorbing solar energy, while most other aerosols (such as sulfur) reflect solar energy and have a cooling effect
Atmospheric gases having three or more atoms in their molecules that tend to absorb infrared radiation given off by the Earth's surface and re-emit it back downward
Combustion of fossil fuels transfers carbon from underground deposits to the atmosphere, and clearing of forests reduces the biosphere's ability to remove carbon dioxide
Humans may have contributed to a net accumulation of greenhouse gases in the atmosphere over the past 250 years, primarily due to the release of carbon in fossil fuels during combustion
Michael Crichton: '"Historically, the claim of consensus has been the first refuge of scoundrels; it is a way to avoid debate by claiming that the matter is already settled."'
Climate scientists can analyze tiny bubbles of atmosphere that collected as ice formed in glaciers, sediment cores, tree rings, and coral reefs to study past climate conditions
Average surface temperatures (both land and ocean) have risen by about 1.1°C in the past 100 years, with most of this increase occurring since the 1970s