Sediment transport between estuarine habitats in San Francisco Bay
We investigate mechanisms of sediment transport, resuspension dynamics in shoals, wave evolution in the shallows, wave attenuation in marshes, and transport of sediment between mudflats and marshes. We produce data sets for calibration of and comparison with sediment transport models, including wave parameters, suspended sediment concentration, and sediment flux.
This research is part of the project, “Sediment Transport in Coastal Environments.”
Objectives
Investigate mechanisms of sediment transport from shoals to channels
Investigate resuspension dynamics in subtidal and intertidal shoals, and determine critical shear stresses for these environments
Investigate wave evolution in the shallows, because of its critical importance to sediment resuspension
Investigate wave attenuation in marshes
Investigate transport of sediment between mudflats and marshes
Produce data sets for calibration of and comparison with sediment transport models, including wave parameters, suspended sediment concentration, and sediment flux.
Accomplishments
Four large deployments (30-40 instruments at 5-8 stations) measuring waves, currents, turbulence, and suspended sediment concentration have been completed: two in South San Francisco Bay, focused on exchange between shoal and channel, in collaboration with UC Berkeley; and two in San Pablo Bay, focused on transport between intertidal and subtidal regions, as part of a post-doctoral research project. See a video on this project. A smaller deployment in Corte Madera Bay was also completed, focused on wave attenuation in the shallows, as part of a larger San Francisco Bay Conservation and Development Commission project.
Learn about all of the “Sediment Transport in Coastal Environments” research studies by choosing a title below.
Sediment Transport in Coastal Environments
San Francisco Bay geomorphology
Below are data releases associated with this project.
Below are multimedia items associated with this project.
Sediment Transport in San Francisco Bay
The Sacramento and San Joaquin Rivers deliver half the amount of sediment they did 50 years ago to San Francisco Bay. Just as sea-level rise is accelerating, the demand for sediment is growing. The amount of sediment supplied to estuaries is important to the fate of shallow water habitats, including mudflats and tidal marshes. In San Francisco Bay, U.S. Geological Survey scientists and...
Below are publications associated with this project.
Bathymetric survey and digital elevation model of Little Holland Tract, Sacramento-San Joaquin Delta, California Bathymetric survey and digital elevation model of Little Holland Tract, Sacramento-San Joaquin Delta, California
Wave attenuation in the shallows of San Francisco Bay Wave attenuation in the shallows of San Francisco Bay
Mechanisms of sediment flux between shallows and marshes Mechanisms of sediment flux between shallows and marshes
Model-based interpretation of sediment concentration and vertical flux measurements in a shallow estuarine environment Model-based interpretation of sediment concentration and vertical flux measurements in a shallow estuarine environment
Lateral baroclinic forcing enhances sediment transport from shallows to channel in an estuary Lateral baroclinic forcing enhances sediment transport from shallows to channel in an estuary
Interactions between waves, sediment, and turbulence on a shallow estuarine mudflat Interactions between waves, sediment, and turbulence on a shallow estuarine mudflat
We investigate mechanisms of sediment transport, resuspension dynamics in shoals, wave evolution in the shallows, wave attenuation in marshes, and transport of sediment between mudflats and marshes. We produce data sets for calibration of and comparison with sediment transport models, including wave parameters, suspended sediment concentration, and sediment flux.
This research is part of the project, “Sediment Transport in Coastal Environments.”
Objectives
Investigate mechanisms of sediment transport from shoals to channels
Investigate resuspension dynamics in subtidal and intertidal shoals, and determine critical shear stresses for these environments
Investigate wave evolution in the shallows, because of its critical importance to sediment resuspension
Investigate wave attenuation in marshes
Investigate transport of sediment between mudflats and marshes
Produce data sets for calibration of and comparison with sediment transport models, including wave parameters, suspended sediment concentration, and sediment flux.
Accomplishments
Four large deployments (30-40 instruments at 5-8 stations) measuring waves, currents, turbulence, and suspended sediment concentration have been completed: two in South San Francisco Bay, focused on exchange between shoal and channel, in collaboration with UC Berkeley; and two in San Pablo Bay, focused on transport between intertidal and subtidal regions, as part of a post-doctoral research project. See a video on this project. A smaller deployment in Corte Madera Bay was also completed, focused on wave attenuation in the shallows, as part of a larger San Francisco Bay Conservation and Development Commission project.
Learn about all of the “Sediment Transport in Coastal Environments” research studies by choosing a title below.
Sediment Transport in Coastal Environments
San Francisco Bay geomorphology
Below are data releases associated with this project.
Below are multimedia items associated with this project.
Sediment Transport in San Francisco Bay
The Sacramento and San Joaquin Rivers deliver half the amount of sediment they did 50 years ago to San Francisco Bay. Just as sea-level rise is accelerating, the demand for sediment is growing. The amount of sediment supplied to estuaries is important to the fate of shallow water habitats, including mudflats and tidal marshes. In San Francisco Bay, U.S. Geological Survey scientists and...
Below are publications associated with this project.