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The evolution of climate cover

The evolution of climate

Chapter 44: FOOTNOTES:
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About This Book

The work surveys geological and meteorological evidence for major past climate changes, reviews paleoclimatology methods and problems of zonal interpretation, examines ice ages and warm intervals, and criticizes the tendency to generalize from limited fossil-correlated horizons. It brings together geology, anthropology, and atmospheric science to propose that changes in land–sea distribution and in land elevation can drive long-term climatic shifts, presents supporting observations and mathematical exposition, and evaluates competing explanations while emphasizing the limitations of the available data and the resulting uncertainties.

FOOTNOTES:

[1] By this term we shall in future understand only that part of it which is responsible for thermal effects.

[2] If the figure of the earth is adjusted to its speed of rotation before the development of ice-sheets, the latter renders it too prolate, and there will be a tendency for readjustment by the transference of mass towards the equator.

[3] This has been the subject of much discussion recently. For a summary see Science Progress, 17, 1922, October, p. 233.

[4] Leverett, F. (see Bibliography).

[5] See reference to Antevs in this connexion.

[6] “The pulse of Asia,” p. 356. See also a new work by E. Huntington, entitled: “Climatic changes.”

[7] “Climatic variations in historic and prehistoric time.”

[8]Sur le prétendu changement du climat européen en temps historique.

[9] Or lemur-like ancestor. There is evidence to show that man’s ancestor was a nocturnal animal, whose food supply was governed by the phases of the moon.

[10] “Scientific monthly,” New York, 4, 1917, pp. 16-26.

[11] “Science progress,” 15, 1920, p. 74.

[12] “Climate and evolution.”

[13] “Civilization and climate.”