No CrossRef data available.
Article contents
Initiation of Deep-Sea Waves of Three Classes: (1) from a Single Displacement; (2) from a Group of Equal and Similar Displacements; (3) by a Periodically Varying Surface-Pressure
Published online by Cambridge University Press: 15 September 2014
Abstract
An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content.
- Type
- Proceedings
- Information
- Copyright
- Copyright © Royal Society of Edinburgh 1906
References
page 407 note * If we continue the argument-curve to the side of the origin for x-negative, we must include large negative values of i in (146): but for simplicity we have confined the argument-curve to positive values of x.
page 416 note * Nature, August 1877, and Brit. Ass. Report, 1877
page 427 note * Remember that downward ordinates in all the curves of figs. 36, 37, 38, 39, correspond to positive values of the quantities represented.
page 428 note * The scale of ordinates of the third, fourth, and fifth curves of fig. 38 is double that of the first and second, indicated on the figure.
page 431 note * Mémoires de l'Institut, 1810. See Gregory's, Examples, p. 480.Google Scholar
page 433 note * The beautiful mathematical discovery, 
seems to have been made by Euler about 1730.
page 433 note † Phil. Mag., October 1871.
page 433 note ‡ See Glaisher, , “On a Class of Definite Integrals,” Phil. Mag., October 1871Google Scholar; and Burgess, , “On the Definite Integral 
” Tram. Roy. Soc. Edin., 1898.Google Scholar