Abstract
The paper addresses the possible role of mathematical models in the analysis of large-scale coastal behaviour (LSCB). The constituent processes (waves, currents, sediment transport) and their interaction with the bottom topography changes (morphodynamics) are considered at various space and time scales. The overall conclusion is, that mathematical modelling has much to add to the analysis and interpretation of large-scale coastal dynamics, especially if it can be integrated with laboratory and field measurements.

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