Inlet wave–current dynamics and interactions are vital to the physical exchanges in a lagoon–
inlet–coastal ocean system. A wave–current coupled model was calibrated and validated …

The circulation in a shallow lagoon–inlet–coastal ocean system is significant to material
transports (eg, debris, pollutants, and larvae). To study surface flows in this system, we …

We examine the relative dispersion and the contribution of tides on the relative diffusivities of
surface drifters in the North Sea. The drifters are released in two clusters, yielding 43 pairs …

While significant studies have been conducted in Intermittently Closed and Open Lakes and
Lagoons (ICOLLs), very few have employed Lagrangian drifters. With recent attention on the …

In this second of two papers, the high spatial resolution cBathy depth estimate algorithm is
extended to account for the existence of currents aligned with the wave directions. The …

A 9 km long tracer plume was created by continuously releasing Rhodamine WT dye for 2.2
h during ebb tide within the southern edge of the main tidal channel at New River Inlet, NC …

Abstract Long Island Sound is a large macrotidal estuary. Connecticut River as the primary
freshwater source enters near the sound's mouth. The summertime pathways of river water …

A near‐shoreline, continuous dye release at an approximately alongshore‐uniform beach
(IB09 experiment) is simulated with the wave‐resolving Boussinesq model funwaveC. The …

Small tide-dominated estuaries are affected by large scale flow structures which combine
with the underlying bed generated smaller scale turbulence to significantly increase the …

In this work we investigated the predictability of the wind‐induced sea surface transport in
coastal areas. The wind fields predicted by two state‐of‐the‐art meteorological models …