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Published online by Cambridge University Press: 15 September 2014
In this paper it is not proposed to discuss in their relations to storms the effects of rain, of the earth's rotation, of areas of high and low pressure external to the storm-area, and of the prevailing westerly winds, which are doubtless occasional factors in the progressive movement of storms. What it is intended to show here is that storms possess in themselves a self-motive power, by which their onward movement over the earth's surface is determined.
page 572 note * “Proceedings of R.S.E.’ vol. viii. p. 613 and p. 614.
page 573 note * “Proceedings,” vol. ix. p. 412.
page 574 note * ‘Proceedings,’ vol. viii. p. 613.
page 574 note † Ibid. vol. viii. p. 614.
page 576 note * See “Journal of Scottish Meteorological Society,” vol. iv. p. 149.
page 577 note * “Proceedings,” vol. viii. p. 613–615.