Trains d’ondes océaniques. Constitution. Propagation. Modes de prédiction
Ocean wave trains. Constitution -Propagation. Methods of prediction. When the sea is being blown up by the wind the agitation consists of a 3 — dimensional ondulating movement. The swell thus produced then becomes more regular, all the while moving forward in the decay area until it takes on an almo...
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| Format: | Article in Journal/Newspaper |
| Language: | French |
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Paris : Société Hydrotechnique de France
1957
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| Online Access: | https://www.persee.fr/doc/jhydr_0000-0001_1957_act_4_1_3335 |