Summary
The A. points out that the confirmation of the theory ofNeumann's significative waves, which differ from those ofSverdrup andMunk, would require observations of an accuracy not yet available. The existence of these waves would not change, anyhow,Sverdrup andMunk's conclusions out of the wind area.
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G. Neumann:Ueber Seegang, Dünung und Wind. Deutsche Hydrographische Zeits., Vol. 3, 1950, p. 40.
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Tenani, M. Relazioni tra la velocità del vento e le caratteristiche del moto ondoso al largo e in costa. Geofisica Pura e Applicata 21, 131–132 (1952). https://doi.org/10.1007/BF01995661
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DOI: https://doi.org/10.1007/BF01995661