James Croll and the astronomical theory of climate change
James Croll (1821-1890) was a Scottish physical scientist who was the leading proponent of an astronomical theory of change] in the nineteenth century. His fundamental insights into the interplay of astronomical and factors] – into cosmic physics and Dynamics] -- were extremely influential. In 1875 Croll published his major book, Climate and Time, a work delayed several years due to ill health, but a work widely admired for the profound impression it produced on geologists around the world. The leading geologist of his day, Charles Lyell], revised his Principles of Geology in response to Croll’s theory.
In 1864, Croll published an article in the Philosophical Magazine “On the Physical Cause of the Change of Climate During Geological Epochs.” In this paper Croll introduced changes in the earth's orbital elements] as likely periodic and extraterrestrial mechanisms for initiating multiple epoch]s.
Croll proposed that the eccentricity of the orbit] was sufficiently great to “account for every extreme of change] evidenced by geology.” His theory of age]s took into account both the precession of the Equinoxes and variations in the shape of the earth's orbit. It predicted that one hemisphere or the other would experience an ice age whenever two conditions occur simultaneously: a markedly elongate orbit, and a Solstice] that occurs far from the sun.
These cosmical factors provided a mechanism for multiple epoch]s and alternating cold and warm periods in each hemisphere. In other words, when the Northern Hemisphere was in the grips of an ice age, the Southern Hemisphere would be in an interglacial. As the earth's orbital elements varied, this situation would eventually be reversed. Feedback mechanisms, such as Effect]s of the ice fields, enhanced formation of cloud and fog, changes in Level], and the mixing and redirection of warm and cold current]s would serve to enhance the climatic changes initiated by the orbital elements.
The astronomical theory of change] emerged between 1864 and 1890 with the work of James Croll. However, because of uncertainties in the timing of age]s and in the Record], and because Croll’s theory predicted glaciation in only one hemisphere, the theory was largely disregarded for at least three decades. The astronomical theory reemerged from Eclipse and was formulated into a mathematical theory of insolation by Milutin Milankovi?] between 1920 and 1941. But even the Theory] “had an uneven run” and was in partial eclipse until the 1960s, in part because of Lags in the climate system] and in part because of the unexplained lack of continental glaciation prior to the Pleistocene. In 1976 the theory received new confirmation from the paleostratigraphic work of James Hayes, John Imbrie, Nicholas Shackelton, and others who documented the astronomical signals in a number of independent proxy climate records.
During Croll’s lifetime the Ice Age] had been discovered and notions of multiple glacial and “Crollean” epoch]s were being debated. Many of the major mechanisms of climatic change had been proposed, if not yet fully explored: changes in Output], changes in the Orbital geometry], geographical changes, and changes in transparency] and composition]. New climate theories were being introduced and new work was being done on Budget]s, Spectroscopy, and the Dioxide] content of the atmosphere. The stratographic sequence had not been worked out and many geologists still thought that glacial “drift” deposits] had been carried by Icebergs. Through such tempestuous theoretical waters, Croll kept a steady course, negotiating between cosmic and terrestrial physics on the one hand (as exemplified by Herschel] and Lord Kelvin]) and geology on the other, as practiced by Lyell], Darwin], and the Geikie brothers.
Editor's Note: This entry is adapted from Rodger Fleming], James Croll in Context: The Encounter between Climate Dynamics and Geology in the Second Half of the Nineteenth Century, History of Meteorology 3 (2006):43-53
Further reading
- Croll, James, 1875. Climate and Time in Their Geological Relations. A theory of secular changes of the earth's climate. New York.
- Fleming, James Rodger, 1998. Historical Perspectives on Climate Change. New York. [[|1=0195078705}}]]
- Irons, James Campbell, 1896. Autobiographical Sketch of James Croll with Memoir of his Life and Work. London.
- Lyell, Charles, 1866-68. Principles of Geology, 10th ed. London.
