This paper summarizes the findings of a workshop convened in the United States in 2018 to
discuss methods in coastal and estuarine modeling and to propose key areas of research …

Estuaries and tidal embayments are partly enclosed coastal bodies of water with a free
connection to the open sea at their tidal inlet and with minimal (tidal embayments) or …

Abstract The Connecticut River is a tidal salt wedge estuary, where advection of sharp
salinity gradients through channel constrictions and over steeply sloping bathymetry leads to …

Abstract The East China Sea (ECS) inner shelf is highly impacted by tropical cyclones. Due
to the limited availability of observations, the sediment dynamics and associated …

It is often assumed that, in short, shallow estuaries, at leading order velocity and elevation
are exactly out of phase, so that duration asymmetries in the rise and fall of the tide should …

Cold water mass (CWM) is a distinct hydrologic phenomenon in summer in worldwide
continental shelf seas. CWM can significantly affect circulation patterns and biogeochemical …

Maintaining accretion and progradation in a mega delta is crucial to its geomorphic stability
and ecology. Extreme riverine floods can disturb hydro-sediment dynamics with great …

Most of the estuarine and ocean bottoms are covered with sediments making this the largest
habitat on our planet. Grain size data of the estuarine sediments are of great importance in …

Shallow, bar‐built estuaries on wave‐dominated coasts in Mediterranean climates
experience an intermittent connection to the ocean. In the presence of low streamflow, their …

Estuarine geomorphology worldwide has greatly changed in the Anthropocene due to
intensive human inferences in river basin and within estuary, which has received increasing …