Motion of water and sediment due to non-breaking waves in the swash zone
A long wave run-up theory is applied to the modelling of wave-induced flow velocities, sediment transport rates and bottom changes in a swash zone. First, the properties of the water tongue motion and the resulting lithodynamic response are analysed theoretically. Next, an attempt is made to run the...
Guardat en:
| Autors principals: | , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Institute of Oceanology of the Polish Academy of Sciences
2012-04-01
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| Col·lecció: | Oceanologia |
| Matèries: | |
| Accés en línia: | http://www.iopan.gda.pl/oceanologia/54_2.html#A3 |
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