Robert Jenkins
Robert Jenkins is a Physical Scientist at the St. Petersburg Coastal and Marine Science Center in St. Petersburg, Florida.
Science and Products
Modeling the Effects of Large-scale Interior Headland Restoration on Tidal Hydrodynamics and Salinity Transport in an Open Coast, Marine-dominant Estuary: Model Input and Results
The effects of large-scale interior headland restoration on tidal hydrodynamics and salinity transport in the Grand Bay, Alabama (AL) estuary was assessed using a two-dimensional Discontinous-Galerkin Shallow Water Equations (DG-SWEM) model. Three restoration alternatives were simulated: 1) no action (herein referred to as na); 2) reconstruction of the Grand Batture Island (herein referred to as G
Modeling the Effects of Interior Headland Restoration on Estuarine Sediment Transport Processes in a Marine-Dominant Estuary: Delft3D Model Output
Assessing habitat change and migration of barrier islands
Dauphin Island Decadal Forecast Evolution Model Inputs and Results
Dauphin Island Decadal Hindcast Model Inputs and Results
Mobile Harbor Navigation Channel Delft3D Model Inputs and Results
Laboratory Observations of Artificial Sand and Oil Agglomerates Video and Velocity Data
Modeling the effects of interior headland restoration on estuarine sediment transport processes in a marine-dominant estuary
Modeling the effects of large-scale interior headland restoration on tidal hydrodynamics and salinity transport in an open coast, marine-dominant estuary
The effects of large-scale interior headland restoration on tidal hydrodynamics and salinity transport in an open coast, marine dominant estuary (Grand Bay, Alabama, U.S.A) are investigated using a two-dimensional model, the Discontinuous-Galerkin Shallow Water Equations Model (DG-SWEM). Three restoration alternatives are simulated for present-day conditions, as well as under 0.5 m of sea level ri
Assessing habitat change and migration of barrier islands
The roles of storminess and sea level rise in decadal barrier island evolution
Development of a modeling framework for predicting decadal barrier island evolution
Application of decadal modeling approach to forecast barrier island evolution, Dauphin Island, Alabama
Development of a process-based littoral sediment transport model for Dauphin Island, Alabama
Effects of proposed navigation channel improvements on sediment transport in Mobile Harbor, Alabama
Laboratory observations of artificial sand and oil agglomerates
Science and Products
Modeling the Effects of Large-scale Interior Headland Restoration on Tidal Hydrodynamics and Salinity Transport in an Open Coast, Marine-dominant Estuary: Model Input and Results
The effects of large-scale interior headland restoration on tidal hydrodynamics and salinity transport in the Grand Bay, Alabama (AL) estuary was assessed using a two-dimensional Discontinous-Galerkin Shallow Water Equations (DG-SWEM) model. Three restoration alternatives were simulated: 1) no action (herein referred to as na); 2) reconstruction of the Grand Batture Island (herein referred to as G
Modeling the Effects of Interior Headland Restoration on Estuarine Sediment Transport Processes in a Marine-Dominant Estuary: Delft3D Model Output
Assessing habitat change and migration of barrier islands
Dauphin Island Decadal Forecast Evolution Model Inputs and Results
Dauphin Island Decadal Hindcast Model Inputs and Results
Mobile Harbor Navigation Channel Delft3D Model Inputs and Results
Laboratory Observations of Artificial Sand and Oil Agglomerates Video and Velocity Data
Modeling the effects of interior headland restoration on estuarine sediment transport processes in a marine-dominant estuary
Modeling the effects of large-scale interior headland restoration on tidal hydrodynamics and salinity transport in an open coast, marine-dominant estuary
The effects of large-scale interior headland restoration on tidal hydrodynamics and salinity transport in an open coast, marine dominant estuary (Grand Bay, Alabama, U.S.A) are investigated using a two-dimensional model, the Discontinuous-Galerkin Shallow Water Equations Model (DG-SWEM). Three restoration alternatives are simulated for present-day conditions, as well as under 0.5 m of sea level ri