River delta degradation has been caused by extraction of natural resources, sediment
retention by reservoirs, and sea-level rise. Despite global concerns about these issues …

Morphodynamic equilibrium is a widely adopted yet elusive concept in the field of
geomorphology of coasts, rivers and estuaries. Based on the Exner equation, an expression …

River‐tide dynamics remain poorly understood, in part because conventional harmonic
analysis (HA) does not cope effectively with nonstationary signals. To explore nonstationary …

At a global scale, delta morphologies are subject to rapid change as a result of direct and
indirect effects of human activity. This jeopardizes the ecosystem services of deltas …

The Wadden Sea is a unique coastal wetland containing an uninterrupted stretch of tidal
flats that span a distance of nearly 500km along the North Sea coast from the Netherlands to …

The fluvial to marine transition zone (FMTZ) is the area of coastal rivers in which
sedimentation is controlled by the interaction of fluvial and marine processes. This study …

Along their fluvial to marine transition zone, tide-dominated river deltas show upstream to
downstream trends in channel width, sinuosity, and depth, which at present have been only …

Understanding the decadal morphodynamic evolution of estuaries and deltas and their
controls is of vital importance regarding management for estuarine function and sustainable …

Tidal wave deformation and tidal asymmetry widely occur in tidal estuaries and lagoons.
Tidal asymmetry has been intensively studied because of its controlling role on residual …

Topographic data in the form of digital elevation models (DEMs) play a significant role in
flood management. Despite the increasing availability of DEMs for large regions, there is a …