CNN’s View of Climate History

Some of you might notice that some other items of interest were left out… feel free to fill in the gaps.
 
A timeline of climate change science

By Matthew Knight for CNN

LONDON, England (CNN) – Climatology was once a small and often overlooked branch of science. But important discoveries made as [early as] the early 19th century have contributed to what is the most important field of scientific study in the world today. Listed below are some key dates in climate change history.

1824
French physicist Joseph Fourier is first to describe a “greenhouse effect” in a paper delivered to Paris’s Académie Royale des Sciences.
1861
Irish physicist John Tyndall carries out research on radiant heat and the absorption of radiation by gases and vapors including CO2 and H2O. He shows that carbon dioxide can absorb in the infrared spectrum, and it can cause a change in temperature. Tyndall famously declares: “The solar heat possesses. . . the power of crossing an atmosphere. But when the heat is absorbed by the planet, it is so changed in quality that the rays emanating from the planet cannot get with the same freedom back into space. Thus the atmosphere admits of the entrance of the solar heat, but checks its exit. The result is a tendency to accumulate heat at the surface of the planet.”
1896
Swedish chemist Svante Arrhenius first proposes the idea of a man-made greenhouse effect. He hypothesizes that the increase in the burning of coal since the beginning of industrialization could lead to an increase in atmospheric CO2 and heat up the earth. Arrhenius was trying to find out why the earth experienced ice ages. He thought the prospect of future generations living “under a milder sky” would be a desirable state of affairs.
1938
British engineer Guy Stewart Callendar compiles temperature statistics in a variety of regions and finds that over the previous century the mean temperature had risen markedly. He also discovers that CO2 levels had risen 10 percent during the same period. He concludes that CO2 was the most likely reason for the rise in temperature.
1955
John Hopkins University researcher Gilbert Plass proves that increased levels of carbon dioxide could raise atmospheric temperature. By 1959 Plass is boldly predicting that the earth’s temperature would rise more than 3 degrees Fahrenheit by the end of the century.
In the same year chemist Hans Suess detects the fossil carbon produced by burning fuels, although he and Roger Revelle - director of the Scripps Institute of Oceanography - declare that the oceans must be absorbing the majority of atmospheric carbon dioxide, they decide to conduct further research.
1958
Revelle and Suess employ geochemist Charles Keeling to continuously monitor CO2 levels in the atmosphere. After only two years of measurements in Antarctica an increase is visible. The graph becomes widely known as the Keeling Curve and becomes an icon of global warming debate and continues to chart the year on year rise in CO2 concentrations to this day.