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James Croll: a scientist ahead of his time

Published online by Cambridge University Press:  08 July 2011

V.A. Bol'shakov ,
A.P. Kapitsa  and
W.G. Rees
V.A. Bol'shakov
Affiliation:
M.V. Lomonosov Moscow State University, Moscow 119991, Russia
A.P. Kapitsa
Affiliation:
M.V. Lomonosov Moscow State University, Moscow 119991, Russia
W.G. Rees
Affiliation:
Scott Polar Research Institute, University of Cambridge, Cambridge CB2 1ER ([email protected])
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Abstract

James Croll (1821–1890) was a Scottish scientist who made major, although still largely unrecognised, contributions to the theory of the effects of variations in the Earth's orbit on the global climate. He was the first to identify the importance of positive feedbacks in the climate system, especially the ice-albedo feedback, and he placed the astrochronological method on a sound footing. Croll's theory was the first to predict multiple ice ages. However, it was unable to place the end of the most recent glaciation more recently than 80,000 years ago, and as evidence accumulated throughout the 19th century for a much more recent date than this Croll's theory fell into neglect. We argue that this was particularly unfortunate since several of his key ideas were forgotten, and that this has delayed the development of the orbital theory of paleoclimate.

Type
Notes
Information
Polar Record , Volume 48 , Issue 2 , April 2012 , pp. 201 - 205
Copyright
Copyright © Cambridge University Press 2011

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References

Adhémar, J.A. 1842. Revolutions de la mer: déluges périodiques. Paris: Carilian-Goeury et V. Dalmont.Google Scholar
Berger, A.L., and Loutre, M.F.. 1991. Insolation values for the climate of the last 10 million years. Quaternary Science Reviews 10: 297–317CrossRefGoogle Scholar
Berger, A.L., Loutre, M.F., and Gallee, H.. 1998. Sensitivity of the LLN climate model to the astronomical and CO2 forcings over the last 200 ky. Climate Dynamics 14: 615–629.CrossRefGoogle Scholar
Bol'shakov, V.A. 2003a. Modern climatic data for the Pleistocene: implications for a new concept of the orbital theory of paleoclimate, Russian Journal of Earth Sciences 5 (2): 125–143 (URL: http://rjes.wdcb.ru/v05/TJE03116/TJE03116.htm).CrossRefGoogle Scholar
Bol'shakov, V.A. 2003b. Novaya konseptsiya orbital'noy teorii paleoklimata [The new concept of the orbital theory of paleoclimate]. Moscow: Moscow State University.Google Scholar
Bol'shakov, V.A. 2008. How long will the ‘precession epoch’ last in terms of Pleistocene glacial cycles? Russian Journal of Earth Sciences 10: ES3004 (doi: 10.2205/2008ES000299).Google Scholar
Croll, J. 1864. On the physical cause of the change of climate during geological epochs. Philosophical Magazine 28:121–137.Google Scholar
Croll, J. 1867. On the change in the obliquity of the ecliptic, its influence on the climate of the polar regions and on the level of the sea. Philosophical Magazine 33: 426–445.Google Scholar
Croll, J., 1875. Climate and time in their geological relations: a theory of secular changes of the Earth's climate. London: Edward Stanford.Google Scholar
Hays, J.D., Imbrie, J., and Shackleton, N.. 1976. Variation in the Earth's orbit: pacemaker of the ice ages. Science 194: 1121–1132.CrossRefGoogle ScholarPubMed
Imbrie, J., 1982. Astronomical theory of the Pleistocene Ice Ages: a brief historical review. Icarus 50: 408–422.CrossRefGoogle Scholar
Imbrie, J., and Imbrie, J.Z.. 1980. Modelling the climatic response to orbital variations. Science 207: 943–953.CrossRefGoogle ScholarPubMed
Imbrie, J., and Imbrie, K.P.. 1986. Ice ages: solving the mystery. Cambridge MA and London: Harvard University Press.Google Scholar
Imbrie, J., Berger, A., Boyle, E.A., Clemens, S.C., Duffy, A., Howard, W.R., Kukla, G., Kutzbach, J., Martinson, D.G., McIntyre, A., Mix, A.C., Molfino, B., Morley, J.J., Peterson, L.C., Pisias, N.G., Prell, W.L., Raymo, M.E., Shackleton, N.J., and Toggweiler, J.R.. 1993. On the structure and origin of major glaciation cycles. 2.The 100,000-year cycle. Paleoceanography 8: 699–735.CrossRefGoogle Scholar
Irons, J.C. (editor). 1896. Autobiographical sketch of James Croll with memoir of his life and work. London: E. Stanford.Google Scholar
Milankovitch, M. 1930. Mathematische Klimalehre und astronomische Theorie der Klimaschwankungen. Berlin: Gebruder Borntraeger (Handbuch der Klimatologie 1).Google Scholar