Summary
The subject is treated, how far the events of motion in the sea can be reproduced by application of methods, which are based on the hydrodynamical differential equations. In particular comparisons between observed and computed sea-levels for the tides in estuaries and in the North-sea are worked out. Furtheron, a method is communicated, which is giving the shape of the sea-surface, when distribution of density is known, without using a layer of no motion. The result shows a remarkable agreement with the topography of the sea-surface in the South-Atlantic given byA. Defant.
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Aus einem Vortrag gehalten am 3. April 1959 auf der 7. Allgem. Versammlung der ≪Società Italiana di Geofisica e Meteorologia≫ (Genova: 3.–5. April 1959).
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Hansen, W. Hydrodynamische Methoden in der Ozeanographie: Beiträge zur Physik der Bewegungsvorgänge im Meere. Geofisica Pura e Applicata 44, 154–167 (1959). https://doi.org/10.1007/BF01997643
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DOI: https://doi.org/10.1007/BF01997643