Synthetic aperture sonar (sas) systems are designed to observe stationary scatterers located
near the sediment interface. Less commonly, a sas system may be used to observe …

The topography between the ocean and marginal sea basins is often complex with narrow
channels and shallow sills. Two-layer exchange flows are usually observed in the channels …

The interfaces between small river plumes and ambient seawater have extremely sharp
horizontal and vertical salinity gradients, often accompanied by velocity shear. It results in …

X‐band marine radar observations and a hindcast simulation from a 3D hydrostatic model
are used to provide an overview of Connecticut River (USA) ebb plume front expansion into …

The lobe‐and‐cleft instability is a widely recognized mechanism leading to along‐front
structure on density current fronts. Early studies based on laboratory and numerical …

Abstract The Connecticut River plume is influenced by energetic ambient tides in the Long
Island Sound receiving waters. The objectives of this modeling study are (a) characterizing …

Tidal intrusion fronts are surface convergences that occur at constrictions in estuaries during
the flood tide, separating incoming higher‐salinity water from lower‐salinity, stratified …

The study analyzes the microwave imaging of shoaling nearshore surface gravity waves
during the process of steepening and breaking over two beaches for a wide range of …

Observations of nearshore waves and wave breaking with two different coherent radars at X-
band and two different beaches are presented and compared. These were mostly under low …