XXV.—On the Hydrodynamical Theory of Seiches
1906; Royal Society of Edinburgh; Volume: 41; Issue: 3 Linguagem: Inglês
10.1017/s0080456800035523
ISSN2053-5945
Autores Tópico(s)Geology and Paleoclimatology Research
Resumo§ 1. The variations of the surface-level of lakes due to the direct action of wind and rain, and the smaller disturbances caused by surface waves, of small or moderate length, due to the action of the wind and the movement of boats and animals, must have been familiar phenomena at all times. The first accurately recorded observation, that lake-levels are subject to a rhythmic variation, similar in some respects to the ocean tides, seems to have been made at Geneva in 1730 by Fatio de Duillier, a well-known Swiss engineer. Owing to the peculiar configuration of the Geneva end of Lake Léman, these variations occasionally reach a magnitude of 5 or even 6 feet; and Duillier mentions that they were known in his time by the local name of “Seiches,” which has now been applied to rhythmic alterations of the level of lakes in general.
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