Sulla natura fisica delle onde interne del lago di Bracciano
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Abstract
It is a well know fact t h a t , at an average depth of 15 m,
during t h e summer and the fall, remarkable internal waves appear in the
lake of Bracciano — as Prof. Caloi has shown — such waves must be explaned
by free oscillations of the surface of thermic jump, which takes place
in the lake in those months.
On the basis of a long series of recordings, taken in two lymnographic
stations operating at the estremes of a diameter of the lake, it was possible
to prove that the Bracciano lake internal waves are of asymmetric type,
according to the theory.
during t h e summer and the fall, remarkable internal waves appear in the
lake of Bracciano — as Prof. Caloi has shown — such waves must be explaned
by free oscillations of the surface of thermic jump, which takes place
in the lake in those months.
On the basis of a long series of recordings, taken in two lymnographic
stations operating at the estremes of a diameter of the lake, it was possible
to prove that the Bracciano lake internal waves are of asymmetric type,
according to the theory.
Article Details
How to Cite
CALOI, P. and MIGANI, M. (1964) “Sulla natura fisica delle onde interne del lago di Bracciano”, Annals of Geophysics, 17(2), pp. 213–220. doi: 10.4401/ag-5207.
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