6: Flujo Oscilatorio
- Page ID
- 89050
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- El aspecto de las ondas gravitacionales superficiales que es relevante para el movimiento de los sedimentos radica en gran medida en el movimiento de ida y vuelta del agua en el fondo: ¿esas corrientes oscilatorias son lo suficientemente fuertes como para arrastrar los sedimentos del fondo? Para conocer la naturaleza de los movimientos del fondo del agua bajo las ondas oscilatorias, lo mejor es comenzar con la teoría de ondas de pequeña amplitud.