A brief history of early climate science

Something a little bit different for this post…. After all the recent controversy over hacked emails, IPCC errors and the British public apparently growing more skeptical about climate science and scientists, it is perhaps interesting to take a step back and look at why we believe that emissions of various gases can influence our climate. There are many comprehensive sources of the historical background to modern climate science, and many of the classic papers are freely available. This is a very brief summary of some of the those first ideas.

Early stages

In the 1820s and 1830s scientists such as Joseph Fourier and Claude Pouillet had questioned what set the temperature of the Earth. They realised that something like the greenhouse effect might exist (Fourier’s 1824 paper talks of trapping ‘non-luminous’ heat, i.e. infra-red radiation) , especially from experiments by Horace-Benedict de Saussure who carried an early ‘solar oven’ (essentially a blackened cork box with various plates of glass as insulators) to the top of Alpine peaks, but they did not yet understand the radiative effects fully.

Understanding ice ages

In 1837, Louis Agassiz, had established that the planet had previously been in an ‘ice age’, and many scientists wanted to know why (Milutin Milankovic did not publish his theories on orbital changes until 1920). It was trying to understand these issues which led John Tyndall to perform his pioneering experiments, published in 1861. Using apparatus such as that pictured below, Tyndall attempted to measure the absorption of various gases (including CO2, N2O and C2H4) and concluded that,

“… an almost inappreciable admixture of any of the hydrocarbon vapours would produce great effects on the terrestrial rays and produce corresponding changes of climate.”

Tyndall's experiment

The work of Tyndall, and others, gave Svante Arrhenius the data needed to make the first climate prediction. In a paper published in 1896, he used simple radiative calculations (done by hand!) to estimate the temperature change caused by changing the constituents of the atmosphere, and concluded that if you doubled the amount of CO2 in the atmosphere you would increase the global temperature by about 5°C (modern estimates are around 3°C). Arrhenius also predicted a polar amplification of any change in climate and an increased land-sea contrast, agreeing with modern evidence, but he had ignored the effect of clouds in his calculations.

In a subsequent review article in 1901, Nils Ekholm concluded that CO2 was the primary cause of geological changes in climate, and discussed European climate variability over the previous few hundred years. He also postulated that atmospheric concentration of CO2 could increase over the coming millennium due to the burning of coal, which would warm the Earth and potentially stop the ice ages, concluding,

“It is too early to judge of how far Man might be capable of thus regulating the future climate. But already the view of such a possibility seems to me so grand that I cannot help thinking that it will afford Mankind hitherto unforeseen means of evolution.”

First detection of modern climate changes

However, Arrenhius’ work remained controversial as arguments over the relative roles of water vapour and CO2 in atmospheric absorption went on. Then, in 1938, the potential influence on global climate was revisited by Guy Callendar. He compiled the first global temperature reconstructions (see figure below) and estimated the part of the changes observed which might be caused by changes in CO2 (the dashed lines). He noted that the recent changes were larger than that predicted, and even considered whether the urban heat island effect was responsible. [We now believe that a mixture of causes (solar changes, CO2 and natural variability) are responsible for this early 20th century warming.]

Callendar's temperature record

Beyond 1940

Hindsight may allow us to pick out these key scientists now, but it cannot have been easy at the time to distinguish between competing theories, particularly with the lack of observations and relatively primitive measurement equipment available. After Callendar, the subsequent few decades brought little consensus, although Gilbert Plass and Roger Revelle made important steps forward. In the 1950s and 1960s, concerns about particulates from burning fossil fuels causing a cooling were significant, but not overwhelming. Charles Keeling began measuring the quantity of CO2 in the atmosphere in 1958, but by the 1980s, the Clean Air Acts had reduced the levels of particulates and the warming began to emerge again. In 1988 the IPCC was born and will publish its 5th Assessment Report in 2013.

It is with great admiration that one reads these early papers, particuarly the obvious dedication with which they approach devoting years to tedious calculations or designing and building new equipment. It is recommended reading for all!

Any comments and corrections are very welcome. This post was first put online on the Department of Meteorology WCD blog.

About Ed Hawkins

Ed Hawkins (twitter: @ed_hawkins) is a climate scientist in NCAS-Climate at the Department of Meteorology, University of Reading. His research interests are in decadal variability and predictability of climate, especially in the Atlantic region, and in quantifying the different sources of uncertainty in climate predictions and impacts. Ed is a Contributing Author to IPCC AR5 and a member of the CLIVAR Scientific Steering Group.
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