Coastal Morphodynamics

Understanding and predicting the changes in the morphology of the coastal zone, including the topography of the sea bed and the shoreline planform, in connection with waves, currents, tides and sea level rise, is a major challenge in geomorphology and coastal engineering. It is an interdisciplinary topic of interest to oceanographers, civil engineers, physical geographers, geologists, physicists and mathematicians..

Coastal morphodynamics is a really challenging topic. The coastal system is an open system exposed to a very complex external forcing (waves, currents, tides, wind, human interventions) at very distinct length and time scales, ranging from meters and seconds (individual waves) up to hundreds of km's and centuries (climate dynamics, geological constraints, anthropic influences). Secondly, it relies on the still very unknown and highly nonlinear sediment transport processes together with hydrodynamics (with turbulence). Finally, strong feedbacks between flow and morphology are essential giving rise to chaos and complexity and the emergence of self-organized behaviour that couples the space and time patterns of the external forcing with those arising from the internal dynamics.

Our research group investigates the fundamental processes coupling hydrodynamics and morphodynamics that drive coastal morphology. In particular, we investigate the dynamics of cross-shore beach profiles, breaker sand bars, shoreline planforms and sand banks. We cover the study of self-organized morphological patterns, such as rhythmic surf zone bars, rip channels, shoreline sand waves and sand ridges in the continental shelf, as well as of the coastal morphological evolution in the context of climate change.